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<!DOCTYPE html>
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<html lang="de-DE">
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<!-- Mirrored from www.geologie.ac.at/rocky-austria/service/download by HTTrack Website Copier/3.x [XR&CO'2014], Thu, 21 Nov 2024 15:46:49 GMT -->
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<!-- Added by HTTrack --><meta http-equiv="content-type" content="text/html;charset=utf-8" /><!-- /Added by HTTrack -->
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<head>
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<!--
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This website is powered by TYPO3 - inspiring people to share!
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TYPO3 is a free open source Content Management Framework initially created by Kasper Skaarhoj and licensed under GNU/GPL.
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TYPO3 is copyright 1998-2024 of Kasper Skaarhoj. Extensions are copyright of their respective owners.
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Information and contribution at https://typo3.org/
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-->
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<base >
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<link rel="icon" href="http://www.geologie.ac.at/typo3conf/ext/gba/Resources/Public/Icons/favicon.ico" type="image/vnd.microsoft.icon">
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<title>Download: Rocky Austria</title>
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<meta http-equiv="x-ua-compatible" content="{$page.meta.compatible}">
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<meta name="viewport" content="{$page.meta.viewport}">
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<meta property="og:title" content="Download">
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<meta name="apple-mobile-web-app-capable" content="{$page.meta.apple-mobile-web-app-capable}">
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<link rel="stylesheet" href="../../typo3temp/assets/css/5ca3b44527a764398332ad2c78342db43fac.css?1648457351" media="all">
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<meta name="viewport" content="width=device-width, initial-scale=1, maximum-scale=1"> <meta http-equiv="X-UA-Compatible" content="IE=edge, chrome=1">
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<link href="../../fileadmin/template-rocky/css/bootstrap.min.css" rel="stylesheet">
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<link href="../../fileadmin/template-rocky/css/jquery.fancybox.css" rel="stylesheet">
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<link href="../../fileadmin/template-rocky/js/helpers/jquery.fancybox-buttons.css" rel="stylesheet">
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<link href="../../fileadmin/template-rocky/css/style.min.css" rel="stylesheet">
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<link href="http://www.geologie.ac.at/fileadmin/template-rocky/img/favicon.ico" rel="icon" type="image/x-icon">
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<![endif]-->
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<script src="../../fileadmin/template-rocky/js/jquery-1.11.1.min.js"></script>
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<script src="../../fileadmin/template-rocky/js/jquery.fancybox.pack.js"></script>
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<script type="text/javascript" src="../../fileadmin/template/js/jquery.textresizer.min.js"></script>
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<script src="../../fileadmin/template-rocky/js/helpers/jquery.fancybox-buttons.js"></script>
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<script src="../../../unpkg.com/popper.js%401.16.1/dist/umd/popper.min.js"></script>
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<script src="../../../unpkg.com/tooltip.js%401.3.3/dist/umd/tooltip.min.js"></script>
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<!-- <script type="text/javascript" src="https://s3.amazonaws.com/cdn.knightlab.com/libs/timeline/latest/js/storyjs-embed.js"></script>-->
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<script src="../../fileadmin/template-rocky/js/script.js"></script>
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<script>
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$(document).ready(function() {
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createStoryJS({
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type: 'timeline',
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width: '800',
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height: '600',
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source: '/fileadmin/template-rocky/timeline/example_json.json',
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embed_id: 'timeline-embed', //OPTIONAL USE A DIFFERENT DIV ID FOR EMBED
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});
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});
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</script>
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<link rel="canonical" href="download.html">
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<a href="../index.html"><img src="../../fileadmin/template-rocky/img/logo.jpg" alt="Rocky"></a>
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<div class="col-md-7">
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<div class="header-maps">
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<a href="#" data-target="landschaften">Landschaften</a> | <a href="#" data-target="bausteine">Bausteine</a>
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<object id="landschaften" class="landschaften map" data="http://www.geologie.ac.at/fileadmin/template-rocky/img/Karte_Landschaften.svg" type="image/svg+xml">
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Ihr Browser kann leider kein SVG darstellen.
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</object>
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<object id="bausteine" class="bausteine map" data="http://www.geologie.ac.at/fileadmin/template-rocky/img/Karte_Bausteine.svg" type="image/svg+xml" style="display:none;">
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Ihr Browser kann leider kein SVG darstellen.
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</object>
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</div>
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<div class="row">
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<div class="col-md-10">
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<nav id="mainnav">
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<ul><li><a href="../landschaften.html">Landschaften</a><ul class="scndLevel clearfix"><li><a href="../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../landschaften/voralpen.html">Voralpen</a></li><li><a href="../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../grundlagen.html">Grundlagen</a><ul class="scndLevel clearfix"><li><a href="../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../bausteine.html">Bausteine</a><ul class="scndLevel clearfix"><li><a href="../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../bausteine/subpennin.html">Subpennin</a></li><li><a href="../bausteine/pennin.html">Pennin</a></li><li><a href="../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul class="scndLevel clearfix"><li><a href="../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../gebirgsbildung.html">Gebirgsbildung</a></li><li class="selected"><a href="../service.html" class="selected">Service</a><ul class="scndLevel clearfix"><li class="selected"><a href="download.html" class="selected">Download</a></li><li><a href="glossar.html">Glossar</a></li></ul></li></ul>
|
||||
|
||||
</nav>
|
||||
<div id="mobile-nav">
|
||||
<ul><li><a href="#">Menü</a><ul><li><a href="../landschaften.html">Landschaften</a><ul><li><a href="../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../landschaften/voralpen.html">Voralpen</a></li><li><a href="../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li class="last"><a href="../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../grundlagen.html">Grundlagen</a><ul><li><a href="../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li class="last"><a href="../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../bausteine.html">Bausteine</a><ul><li><a href="../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../bausteine/subpennin.html">Subpennin</a></li><li><a href="../bausteine/pennin.html">Pennin</a></li><li><a href="../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../bausteine/meliatikum.html">Meliatikum</a></li><li class="last"><a href="../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../entwicklungsgeschichte/neogen.html">Neogen</a></li><li class="last"><a href="../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../gebirgsbildung.html">Gebirgsbildung</a></li><li class="last"><a href="../service.html" class="active">Service</a><ul><li><a href="download.html" class="selected">Download</a></li><li class="last"><a href="glossar.html">Glossar</a></li></ul></li></ul></li></ul>
|
||||
</div>
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||||
</div>
|
||||
<div class="col-md-2">
|
||||
<div class="container-right-top clearfix">
|
||||
<div id="language">
|
||||
<ul></ul>
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||||
</div>
|
||||
<div id="textSizer">
|
||||
<div class="fontSize hidden-sm hidden-xs" id="fontsize">
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||||
<p>
|
||||
<a href="#nogo" class="">
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||||
<span class="medium">A</span>
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||||
</a>
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||||
<a href="#nogo" class="">
|
||||
<span class="large">A</span>
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||||
</a>
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</p>
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</div>
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</div>
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</div>
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||||
<div class="container-right-bottom">
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||||
<div class="search-container">
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||||
<!--<form action="index.php?id=803" method="post" id="indexedsearch">
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<input type="hidden" name="tx_indexedsearch[sections]" value="0">
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||||
<input name="tx_indexedsearch[submit_button]" value="Search" type="hidden">
|
||||
<input name="tx_indexedsearch[sword]" placeholder="Suchbegriff" id="search-field" type="text">
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||||
<input type="image" src="/fileadmin/template-rocky/img/search.png" id="search-button" class="searchButton" alt="Search" title="Search">
|
||||
</form>-->
|
||||
<form method="get" id="form_kesearch_pi1" name="form_kesearch_pi1" action="http://www.geologie.ac.at/rocky-austria/suche/">
|
||||
<fieldset class="kesearch_searchbox">
|
||||
<!-- <input type="hidden" name="id" value="803"> -->
|
||||
<!-- <input type="text" id="ke_search_sword" name="tx_kesearch_pi1[sword]" value="" placeholder="Suchbegriff" onfocus="if (this.value == 'Suchbegriff') { this.value = ''; }" onblur="if (this.value == '') { this.value = 'Suchbegriff'; }">
|
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<input type="image" src="../../fileadmin/template-rocky/img/search.png" id="search-button" class="searchButton" alt="Search" title="Suche"> -->
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||||
<input id="kesearchpagenumber" type="hidden" name="tx_kesearch_pi1[page]" value="1">
|
||||
<input id="resetFilters" type="hidden" name="tx_kesearch_pi1[resetFilters]" value="0">
|
||||
<input id="sortByField" type="hidden" name="tx_kesearch_pi1[sortByField]" value="">
|
||||
<input id="sortByDir" type="hidden" name="tx_kesearch_pi1[sortByDir]" value="">
|
||||
</fieldset>
|
||||
</form>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
|
||||
<div class="row custom-row" id="pageWrap">
|
||||
|
||||
<div class="col-md-3 custom-column">
|
||||
<div id="sidebar" class="content">
|
||||
|
||||
<div id="c13130" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
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||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
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</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
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</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
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||||
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||||
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||||
</div>
|
||||
</div>
|
||||
<div class="col-md-9 custom-column">
|
||||
<div id="maincontent-title" class="content">
|
||||
|
||||
<div id="c12372" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Download
|
||||
</span></h1><h2 class="">
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||||
Graphiken als Vektor-PDF
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||||
</h2></div>
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||||
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||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
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||||
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||||
<div id="c12968" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
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||||
#start-right h3, #sidebar h3, #sidebar h2 {
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||||
margin-top: 0;
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||||
font-size: 1.2em;
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||||
font-weight:normal;
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||||
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||||
}
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||||
#maincontent h3 {
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||||
font-size: 1.2em;
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||||
font-weight:normal;
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||||
color: #606c65 !Important;
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||||
}
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||||
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||||
#maincontent-title h1.csc-firstHeader {
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||||
font-size: 2.2em !important;
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||||
}
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||||
#maincontent-title h2 {
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||||
color: #606c65;
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||||
margin-top: 0;
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||||
font-size: 1.6em;
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||||
margin-top: 0;
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||||
padding-top: 0;
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||||
}
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||||
p {
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||||
margin-top: 0;
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||||
}
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||||
</style></div>
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||||
|
||||
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||||
<div id="c13441" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"></div>
|
||||
|
||||
|
||||
<div id="c12910" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-20">
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||||
<h3>Geologie von Österreich</h3><p><a href="./uebersichtskarte_oesterreich.pdf" title="Öffnet PDF in neuem Fenster" target="_blank" class="download">
|
||||
<span class="link-prefix">» </span>Geolog. Übersichtskarte von Österreich</a> PDF 2,6 MB<br><a href="./profile_uebersichtskarte_oesterreich.pdf" title="Öffnet PDF in neuem Fenster" target="_blank" class="download"><span class="link-prefix">» </span>Profile zur Geolog. Übersichtskarte</a> PDF 1,5 MB</p>
|
||||
<h3>Grundlagen</h3><p>Plattentektonik<br><a href="./plattentektonik.pdf" title="Öffnet PDF in neuem Fenster" target="_blank" class="download">
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||||
<span class="link-prefix">» </span>Plattentektonik und Schalenbau der Erde</a> PDF 2,3 MB</p><p>Gesteinskreislauf<br><a href="./metamorphose_gesteine.pdf" title="Öffnet PDF in neuem Fenster" target="_blank" class="download">
|
||||
<span class="link-prefix">» </span>Metamorphose der Gesteine</a> PDF 1,6 MB <br><a href="./gesteinskreislauf.pdf" title="Öffnet PDF in neuem Fenster" target="_blank" class="download">
|
||||
<span class="link-prefix">» </span>Gesteinskreislauf</a> PDF 8,1 MB</p><p>Fossilien<br><a href="./zeitspirale_ohne_beschriftung.pdf" title="Öffnet PDF in neuem Fenster" target="_blank" class="download">
|
||||
<span class="link-prefix">» </span>Zeitspirale ohne Beschriftung </a>PDF 7 KB<br><a href="./zeitspirale_mit_beschriftung.pdf" title="Öffnet PDF in neuem Fenster" target="_blank" class="download">
|
||||
<span class="link-prefix">» </span>Zeitspirale mit Beschriftung</a> PDF 11 KB<br><a href="./zeitspirale_mit_fossilien.pdf" title="Öffnet PDF in neuem Fenster" target="_blank" class="download">
|
||||
<span class="link-prefix">» </span>Zeitspirale mit Fossilien</a> PDF 13,3 MB</p></div>
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||||
|
||||
<div id="c12930" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-20"><h3>Bausteine</h3>
|
||||
<p><a href="./welt_palaeogeographie_alpenkarte_profil_.pdf" title="Öffnet PDF in neuem Fenster" target="_blank" class="download">
|
||||
<span class="link-prefix">» </span>Paläogeographie, Alpenkarte, -profil</a> PDF 9,8 MB</p></div>
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||||
|
||||
|
||||
<div id="c12932" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-20"><h3>Entwicklungsgeschichte</h3>
|
||||
<p><a href="./stratigraphische_tabelle_2022.pdf" title="Öffnet PDF in neuem Fenster" target="_blank">
|
||||
<span class="link-prefix">» </span>Stratigraphische Tabelle 2022</a> PDF 1 MB</p><p>(Prä-)Kambrium<br>
|
||||
<a href="./01_Prae-Kambrium/welt_spaetes_kambrium.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank">
|
||||
<span class="link-prefix">» </span>Erde im späten Kambrium</a> PDF 159 KB</p><p>Ordoviz, Silur, Devon<br><a href="./welt_spaetes_silur.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank">
|
||||
<span class="link-prefix">» </span>Erde im späten Silur</a> PDF 143 KB<br> <a href="./welt_spaetes_devon.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank">
|
||||
<span class="link-prefix">» </span>Erde im späten Devon</a> PDF 154 KB</p><p>Karbon<br><a href="./welt_karbon.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank">
|
||||
<span class="link-prefix">» </span>Erde im Karbon</a> PDF 149 KB</p><p>Perm<br><a href="./welt_fruehes_perm.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Erde im frühen Perm</a> PDF 77 KB</p><p>Trias<br><a href="./welt_obertrias.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Erde in der späten Trias</a> PDF, 76 KB<br><a href="./karte_trias.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Paläogeographie in der späten Trias</a> PDF 1 MB</p><p>Jura<br><a href="./welt_oberjura.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Erde im späten Jura</a> PDF 79 KB<br><a href="./karte_jura.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Paläogeographie im späten Jura</a> PDF 2,9 MB</p><p>Kreide<br><a href="./welt_unterkreide.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Erde in der frühen Kreide</a> PDF 79 KB<br><a href="./karte_unterkreide.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Paläogeographie in der frühen Kreide</a> PDF 3 MB<br><a href="./welt_oberkreide.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Erde in der späten Kreide</a> PDF 127 KB<br><a href="./karte_oberkreide.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Paläogeographie in der späten Kreide</a> PDF 3,2 MB</p><p>Paläogen<br><a href="./welt_spaete_palaeogen.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Erde im späten Paläogen</a> PDF 136 KB<br><a href="./karte_palaeogen.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Paläogeographie im späten Paläogen</a> PDF 1 MB<br><a href="./augensteinlandschaft_spaetes__palaeogen.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Augensteinlandschaft im späten Paläogen</a> PDF 1,4 MB</p><p>Neogen<br><a href="./extrusion_ostalpen.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Extrusion der Ostalpen</a> PDF 1,5 MB</p><p>Quartär<br><a href="./eiszeitkarte.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Eiszeitkarte</a> PDF 4,1 MB<br><a href="./erdbebenkarte.pdf" title="Öffnet PDF in neuem Fenster" class="download" target="_blank"><span class="link-prefix">» </span>Erdbebenkarte</a> PDF 3,1 MB</p></div>
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|
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|
||||
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<ul><li><a href="#">Menü</a><ul><li><a href="../landschaften.html">Landschaften</a><ul><li><a href="../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../landschaften/voralpen.html">Voralpen</a></li><li><a href="../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li class="last"><a href="../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../grundlagen.html">Grundlagen</a><ul><li><a href="../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li class="last"><a href="../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../bausteine.html">Bausteine</a><ul><li><a href="../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../bausteine/subpennin.html">Subpennin</a></li><li><a href="../bausteine/pennin.html">Pennin</a></li><li><a href="../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../bausteine/meliatikum.html">Meliatikum</a></li><li class="last"><a href="../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../entwicklungsgeschichte/neogen.html">Neogen</a></li><li class="last"><a href="../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../gebirgsbildung.html">Gebirgsbildung</a></li><li class="last"><a href="../service.html" class="active">Service</a><ul><li><a href="download.html">Download</a></li><li class="last"><a href="glossar.html" class="selected">Glossar</a></li></ul></li></ul></li></ul>
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<span class="medium">A</span>
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<input name="tx_indexedsearch[sword]" placeholder="Suchbegriff" id="search-field" type="text">
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<form method="get" id="form_kesearch_pi1" name="form_kesearch_pi1" action="https://www.geosphere.at/rocky-austria/suche/">
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<fieldset class="kesearch_searchbox">
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<!-- <input type="hidden" name="id" value="803"> -->
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<div id="c13129" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
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Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
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</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
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<div id="c12353" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
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Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
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</h2></div>
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<div id="maincontent" class="content">
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#start-right h3, #sidebar h3, #sidebar h2 {
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<div id="c12887" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><b>A</b></td><td><a href="glossar/glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar/glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar/glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar/glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar/glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar/glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar/glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar/glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar/glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar/glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar/glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar/glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar/glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar/glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar/glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar/glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar/glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar/glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar/glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar/glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar/glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12366" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Abschiebung:</h3><p>Geneigte <a href="glossar/glossar-s.html#c12734" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Störung</a>, an der ein <a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>spaket nach unten versetzt wurde. Entsteht durch Dehnung der <a href="glossar/glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12546" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Adria:</h3><p>Ein Stück kontinentaler <a href="glossar/glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphäre</a>, das seit der frühen Oberkreide einen Teil der Adriatischen Platte bildet. Davor war dieses Stück ein Fortsatz am Nordrand des heutigen afrikanischen Kontinents, der auch als „Adriatischer Sporn“ bezeichnet wird. Seit der Öffnung des <a href="glossar/glossar-p.html#c12688" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Penninischen Ozeans</a> wurde der „Adriatische Sporn“ bzw. die <a href="glossar/glossar-k.html#c12641" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kontinentale Kruste</a> der Adriatischen Platte zeitweise vom Meer überflutet und bildete dabei den Adriatischen Schelf.</p></div>
|
||||
|
||||
|
||||
<div id="c12547" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Akkretion:</h3><p>Anschoppung von <a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen </a>bei einer <a href="glossar/glossar-s.html#c12736" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Subduktion</a>, wobei sich ein Anwachskeil bildet.</p></div>
|
||||
|
||||
|
||||
<div id="c12758" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Akkretionskeil:</h3><p>Anschoppung (<a href="glossar.html#c12547" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Akkretion</a>) von Gesteinen, die in einer Subduktionszone von einer ozeanischen Lithosphärenplatte abgeschert werden.</p></div>
|
||||
|
||||
|
||||
<div id="c12548" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Allochthon:</h3><p>Vom Bildungsort entfernt, durch Transportvorgänge in fremde Umgebung verbracht. Im kleineren Maßstab können dies <a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>bruchstücke, Gerölle und Gletschergeschiebe (<a href="glossar/glossar-e.html#c12586" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erratischer Block</a>; <a href="glossar/glossar-g.html#c12602" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Geschiebe</a>) sein, im größeren Maßstab Rutschmassen (<a href="glossar/glossar-r.html#c12710" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Rutschung</a>) oder <a href="glossar/glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Decken</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12549" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Alpidische Gebirgsbildung:</h3><p>Nach den Alpen benannte Entstehung von heutigen Gebirgen mit zahlreichen Einzelphasen vom späten Jura bis ins Neogen.</p></div>
|
||||
|
||||
|
||||
<div id="c12550" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Amethyst:</h3><p>Violette Varietät von <a href="glossar/glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12551" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Ammoniten:</h3><p>Ausgestorbene Teilgruppe der ausschließlich <a href="glossar/glossar-m.html#c12658" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>marin </a>lebenden Kopffüßer mit mehr als 1500 bekannten Gattungen und 30 – 40 000 Arten. Sie stellen seit ihrem ersten Auftreten im Unterdevon bis zu ihrem Aussterben am Ende der Kreide eine große Zahl von <a href="glossar/glossar-l.html#c12650" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Leitfossilien</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12552" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Amphibol-Gruppe:</h3><p>Zumeist dunkel gefärbte, stängelige, <a href="glossar/glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikatische </a>Minerale, die Aluminium, Eisen, Magnesium, Kalzium, Natrium und Wasser enthalten. Sie sind eine wichtige <a href="glossar/glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteinsbildende </a><a href="glossar/glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>gruppe in der <a href="glossar/glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12553" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Amphibolit:</h3><p><a href="glossar/glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a><a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, welches hauptsächlich aus <a href="glossar.html#c12552" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Amphibol </a>und <a href="glossar/glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plagioklas </a>besteht. <a href="glossar/glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a>, <a href="glossar/glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pyroxen</a>, <a href="glossar/glossar-g.html#c12612" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Granat </a>und <a href="glossar/glossar-e.html#c12582" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Epidot </a>können vorkommen.</p></div>
|
||||
|
||||
|
||||
<div id="c12554" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Amphibolitfazies:</h3><p>Bedingungen der mittelgradigen <a href="glossar/glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphose </a>mit 450 – 700 °C und 0,2 – 1,2 GPa Druck.</p></div>
|
||||
|
||||
|
||||
<div id="c12555" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Andesit:</h3><p><a href="glossar/glossar-i.html#c12420" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Intermediäres</a><a href="glossar/glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>vulkanisches</a><a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, welches sich aus <a href="glossar/glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plagioklas</a>, <a href="glossar/glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pyroxen</a>, <a href="glossar/glossar-h.html#c12622" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Hornblende</a> und mitunter <a href="glossar/glossar-b.html#c12755" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Biotit</a> zusammensetzt.</p></div>
|
||||
|
||||
|
||||
<div id="c12556" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Aragonit:</h3><p><a href="glossar/glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>name für Kalzium<a href="glossar/glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>karbonat</a> (CaCO<sub>3</sub>), chemisch ident mit <a href="glossar/glossar-k.html#c12756" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalzit</a>, unterscheidet sich aber in der Anordnung der Atome im Kristallgitter (<a href="glossar/glossar-k.html#c12645" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristall</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c13229" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Arides Klima:</h3><p>Bei aridem Klima ist die Verdunstung größer als der Niederschlag, sodass sich keine dauerhaften Gewässer bilden können.</p></div>
|
||||
|
||||
|
||||
<div id="c12557" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Asthenosphäre bzw. Asthenosphärischer Mantel:</h3><p>Zone geringer Materialfestigkeit im oberen <a href="glossar/glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdmantel</a> unterhalb der <a href="glossar/glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphäre</a> (10 – 200 km) bis in eine Tiefe von 660 km.</p></div>
|
||||
|
||||
|
||||
<div id="c12558" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Augit:</h3><p>Dunkel gefärbtes <a href="glossar/glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikatisches</a><a href="glossar/glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a> der <a href="glossar/glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pyroxen-Gruppe</a>, das <a href="glossar/glossar-k.html#c12756" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalzium</a>, Eisen und Magnesium enthält. Findet sich verbreitet in <a href="glossar/glossar-b.html#c12563" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>basischen</a> und <a href="glossar/glossar-i.html#c12420" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>intermediären</a><a href="glossar/glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>vulkanischen</a><a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12559" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Augensteine:</h3><p>Gerölle aus <a href="glossar/glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kristallinen</a><a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen</a> der Zentralalpen, auf Hochflächen bzw. umgelagert in Höhlen der Nördlichen Kalkalpen; <a href="glossar/glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erosions</a>relikte einstiger Flussablagerungen aus dem Paläogen.</p></div>
|
||||
|
||||
|
||||
<div id="c12560" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-170"><h3>Autochthon:</h3><p>An Ort und Stelle entstanden und verblieben. Für nur leicht verschobene, noch in unmittelbarer Verbindung zu ihrem Bildungsort stehende Objekte wird der Begriff parautochthon benutzt.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
||||
<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
|
||||
<div id="timeline-embed"></div>
|
||||
</div>
|
||||
</div>
|
||||
|
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<div class="container-fluid footer">
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<div class="row footer-menu" id="footer">
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<ul><li class="first col-md-2 col-sm-12"><a href="../landschaften.html">Landschaften</a><ul><li><a href="../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../landschaften/voralpen.html">Voralpen</a></li><li><a href="../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../grundlagen.html">Grundlagen</a><ul><li><a href="../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../bausteine.html">Bausteine</a><ul><li><a href="../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../bausteine/subpennin.html">Subpennin</a></li><li><a href="../bausteine/pennin.html">Pennin</a></li><li><a href="../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../bausteine/molasse.html">Molasse</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../gebirgsbildung.html">Gebirgsbildung</a></li><li class="first col-md-2 col-sm-12"><a href="../service.html">Service</a><ul><li><a href="download.html">Download</a></li><li><a href="glossar.html">Glossar</a></li></ul></li></ul>
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<div class="row">
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<img alt="Link zu www.geologie.ac.at" src="../../fileadmin/template-rocky/img/logo.013b0f3d.svg" width="160">
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309
rocky-austria/service/glossar/glossar-b.html
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<base >
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<link rel="stylesheet" href="../../../../use.fontawesome.com/releases/v5.0.13/css/all.css" integrity="sha384-DNOHZ68U8hZfKXOrtjWvjxusGo9WQnrNx2sqG0tfsghAvtVlRW3tvkXWZh58N9jp" crossorigin="anonymous">
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$(document).ready(function() {
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createStoryJS({
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source: '/fileadmin/template-rocky/timeline/example_json.json',
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embed_id: 'timeline-embed', //OPTIONAL USE A DIFFERENT DIV ID FOR EMBED
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<ul><li><a href="#">Menü</a><ul><li><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li class="last"><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li class="last"><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li class="last"><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li class="last"><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="last"><a href="../../service.html" class="active">Service</a><ul><li><a href="../download.html">Download</a></li><li class="last"><a href="../glossar.html" class="active">Glossar</a></li></ul></li></ul></li></ul>
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<span class="medium">A</span>
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<form method="get" id="form_kesearch_pi1" name="form_kesearch_pi1" action="https://www.geosphere.at/rocky-austria/suche/">
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<div id="sidebar" class="content">
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<div id="c13153" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
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||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
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||||
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|
||||
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|
||||
<div id="maincontent-title" class="content">
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||||
<div id="c12980" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
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||||
|
||||
|
||||
</div>
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||||
<div id="maincontent" class="content">
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<div id="c12978" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
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#start-right h3, #sidebar h3, #sidebar h2 {
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#maincontent h3 {
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color: #606c65 !Important;
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#maincontent-title h1.csc-firstHeader {
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<div id="c12888" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><b>B</b></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12759" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Bankung:</h3><p>Deutliche Gliederung einer <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>abfolge durch Schichtfugen. Die einzelnen Lagen überschreiten eine Dicke von 1 cm und können bis einige Meter erreichen.</p></div>
|
||||
|
||||
|
||||
<div id="c12378" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Baltica:</h3><p>Ehemaliger, frühpaläozoischer Kontinent, der heute als Teil von Eurasien weite Gebiete Nordost- und Osteuropas aufbaut, die von Skandinavien, dem Baltikum und der Ukraine bis zum Ural reichen.</p></div>
|
||||
|
||||
|
||||
<div id="c12561" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Bänderschluff:</h3><p>Im Millimeter-Rhythmus geschichtete, feinkörnige Seeablagerung, die vor allem in Schmelzwasserbecken am Gletscherrand auftritt.</p></div>
|
||||
|
||||
|
||||
<div id="c12562" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Basalt:</h3><p>Dunkles, <a href="glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>vulkanisches</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, welches sich aus <a href="glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plagioklas</a> und <a href="glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pyroxen</a> zusammensetzt. <a href="glossar-o.html#c12676" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Olivin</a> und untergeordnet Foide (<a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a> ähnlich den <a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Feldspaten</a>, jedoch mit weniger SiO<sub>2</sub>) oder <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a> können vorkommen. Bestimmte Basalte sind typisch für die <a href="glossar-o.html#c12681" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>ozeanische Kruste</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12563" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Basisches Gestein:</h3><p><a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatisches</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> mit einem verhältnismäßig geringen SiO<sub>2</sub>-Gehalt von 45 – 52 %; das vorhandene SiO2 ist in <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikatischen</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineralen</a> gebunden, sodass nur ausnahmsweise geringe Mengen an <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a> kristallisieren.</p></div>
|
||||
|
||||
|
||||
<div id="c12564" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Bergsturz:</h3><p>Plötzliche Fels- und Schuttbewegung aus steilen Bergflanken, bei welcher die bewegte Gesteinsmasse mindestens ein Volumen von 1 000 000 m<sup>3</sup> besitzt. Das Material verliert während der Bewegung den inneren Zusammenhang, kann sich großräumig ähnlich einer Flüssigkeit verhalten und sogar an gegenüberliegenden Hängen „aufbranden“.</p></div>
|
||||
|
||||
|
||||
<div id="c12755" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Biotit:</h3><p>Dunkles, eisenreiches <a href="glossar-g.html#c12607" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Glimmermineral</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12565" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Blauschiefer:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, dessen blaue Farbe durch die Anwesenheit von natriumhältigem <a href="../glossar.html#c12552" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Amphibol</a> bedingt ist. Entsteht durch druckbetonte <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphose</a> bei einer <a href="glossar-s.html#c12736" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Subduktion</a> unter hohem Druck (0,7 – 1,6 GPa), aber vergleichsweise niedriger Temperatur (300 – 500 °C).</p></div>
|
||||
|
||||
|
||||
<div id="c12566" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Bodenfließen:</h3><p>Hangabwärtsbewegung der obersten lockeren und wasserdurchtränkten Ablagerungen und <a href="glossar-v.html#c12752" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Verwitterungsprodukte</a>, verbreitet über Dauerfrostböden (<a href="glossar-p.html#c12690" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Permafrost</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12567" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Böhmische Masse:</h3><p>Informeller Begriff für eine Mittelgebirgslandschaft in Mitteleuropa; der österreichische Anteil umfasst Mühl- und Waldviertel.</p></div>
|
||||
|
||||
|
||||
<div id="c12568" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Brackisch:</h3><p>Bezeichnung für Meerwasser mit geringem Salzgehalt.</p></div>
|
||||
|
||||
|
||||
<div id="c12569" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Braunkohle:</h3><p>Braunes, organisches <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a> mit definiertem Brennwert, Feuchtigkeitsund Kohlenstoffgehalt.</p></div>
|
||||
|
||||
|
||||
<div id="c12570" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Brekzie:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klastisches</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a> mit überwiegend kantigen Komponenten, die größer als 2 mm sind. Stellt das verfestigte Äquivalent von Schutt dar.</p></div>
|
||||
|
||||
|
||||
<div id="c12760" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Bruch:</h3><p>Bezeichnung im <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>geologischen</a> Sprachgebrauch für eine steil stehende <a href="glossar-s.html#c12734" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Störung</a>, an der es zu vertikalen Relativbewegungen der angrenzenden <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>körper kommt.</p></div>
|
||||
|
||||
|
||||
<div id="c12761" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-80"><h3>Bündnerschiefer:</h3><p>Bezeichnung für <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteine</a> (<a href="glossar-s.html#c12717" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a>), die gleicher Art in Graubünden in der Schweiz auftreten.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
||||
<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
|
||||
<div id="timeline-embed"></div>
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||||
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|
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273
rocky-austria/service/glossar/glossar-c.html
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273
rocky-austria/service/glossar/glossar-c.html
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@ -0,0 +1,273 @@
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<!DOCTYPE html>
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<base >
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<link rel="stylesheet" href="../../../../use.fontawesome.com/releases/v5.0.13/css/all.css" integrity="sha384-DNOHZ68U8hZfKXOrtjWvjxusGo9WQnrNx2sqG0tfsghAvtVlRW3tvkXWZh58N9jp" crossorigin="anonymous">
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<link href="https://www.geosphere.at/fileadmin/template-rocky/img/favicon.ico" rel="icon" type="image/x-icon">
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$(document).ready(function() {
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createStoryJS({
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height: '600',
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source: '/fileadmin/template-rocky/timeline/example_json.json',
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embed_id: 'timeline-embed', //OPTIONAL USE A DIFFERENT DIV ID FOR EMBED
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<a href="../../index.html"><img src="../../../fileadmin/template-rocky/img/logo.jpg" alt="Rocky"></a>
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<div class="header-maps">
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<div class="switch">
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<a href="#" data-target="landschaften">Landschaften</a> | <a href="#" data-target="bausteine">Bausteine</a>
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<object id="landschaften" class="landschaften map" data="../../fileadmin/template-rocky/img/Karte_Landschaften.svg" type="image/svg+xml">
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Ihr Browser kann leider kein SVG darstellen.
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||||
</div>
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||||
</div>
|
||||
<div class="col-md-2">
|
||||
<div class="container-right-top clearfix">
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||||
<div id="language">
|
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<ul></ul>
|
||||
</div>
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||||
<div id="textSizer">
|
||||
<div class="fontSize hidden-sm hidden-xs" id="fontsize">
|
||||
<p>
|
||||
<a href="#nogo" class="">
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||||
<span class="medium">A</span>
|
||||
</a>
|
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<a href="#nogo" class="">
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<span class="large">A</span>
|
||||
</a>
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||||
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||||
</div>
|
||||
</div>
|
||||
<div class="container-right-bottom">
|
||||
<div class="search-container">
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<!--<form action="index.php?id=803" method="post" id="indexedsearch">
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<input type="hidden" name="tx_indexedsearch[sections]" value="0">
|
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<input name="tx_indexedsearch[submit_button]" value="Search" type="hidden">
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<input name="tx_indexedsearch[sword]" placeholder="Suchbegriff" id="search-field" type="text">
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<input type="image" src="/fileadmin/template-rocky/img/search.png" id="search-button" class="searchButton" alt="Search" title="Search">
|
||||
</form>-->
|
||||
<form method="get" id="form_kesearch_pi1" name="form_kesearch_pi1" action="https://www.geosphere.at/rocky-austria/suche/">
|
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<fieldset class="kesearch_searchbox">
|
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|
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<!-- <input type="text" id="ke_search_sword" name="tx_kesearch_pi1[sword]" value="" placeholder="Suchbegriff" onfocus="if (this.value == 'Suchbegriff') { this.value = ''; }" onblur="if (this.value == '') { this.value = 'Suchbegriff'; }">
|
||||
<input type="image" src="../../../fileadmin/template-rocky/img/search.png" id="search-button" class="searchButton" alt="Search" title="Suche"> -->
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||||
<input id="kesearchpagenumber" type="hidden" name="tx_kesearch_pi1[page]" value="1">
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<input id="resetFilters" type="hidden" name="tx_kesearch_pi1[resetFilters]" value="0">
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<input id="sortByField" type="hidden" name="tx_kesearch_pi1[sortByField]" value="">
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<input id="sortByDir" type="hidden" name="tx_kesearch_pi1[sortByDir]" value="">
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||||
</form>
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||||
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||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
|
||||
<div class="row custom-row" id="pageWrap">
|
||||
|
||||
<div class="col-md-3 custom-column">
|
||||
<div id="sidebar" class="content">
|
||||
|
||||
<div id="c13154" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
|
||||
|
||||
</div>
|
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</div>
|
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<div class="col-md-9 custom-column">
|
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<div id="maincontent-title" class="content">
|
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|
||||
<div id="c12386" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
|
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<div id="c12981" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
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#start-right h3, #sidebar h3, #sidebar h2 {
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#maincontent-title h1.csc-firstHeader {
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|
||||
|
||||
|
||||
<div id="c12384" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Cadomisches Ereignis:</h3><p>Entstehung von Gebirgen am Nordrand des sich formierenden Großkontinents <a href="glossar-g.html#c12610" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gondwana</a> vom Neoproterozoikum bis ins Kambrium.</p></div>
|
||||
|
||||
|
||||
<div id="c12571" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Chlorit:</h3><p>Grünliches Schicht<a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikat</a>, eisenhältig und blättchenförmig.</p></div>
|
||||
|
||||
|
||||
<div id="c12762" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-20"><h3>Cystoideen:</h3><p>Ausgestorbene Tiergruppe des Paläozoikums, die mit den Seeigeln und Seesternen verwandt ist.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
||||
<div class="toggle-content">
|
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<h1>Österreichs geologische Entwicklungsgeschichte</h1>
|
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|
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<ul><li class="first col-md-2 col-sm-12"><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="first col-md-2 col-sm-12"><a href="../../service.html">Service</a><ul><li><a href="../download.html">Download</a></li><li><a href="../glossar.html">Glossar</a></li></ul></li></ul>
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source: '/fileadmin/template-rocky/timeline/example_json.json',
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<div id="c13155" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
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Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
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</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
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<div id="c12392" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
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Glossar
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</span></h1><h2 class="">
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Begriffe von A - Z
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<div id="c12890" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><b>D</b></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12390" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Decke:</h3><p>Großräumiger, im Verhältnis zu seiner Dicke seitlich weit ausgedehnter <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>verband, der von seiner ursprünglichen Unterlage abgelöst und über (mindestens) einige Kilometer auf fremden Untergrund geschoben (<a href="glossar-u.html#c12486" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Überschiebung</a>, <a href="../glossar.html#c12366" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Abschiebung</a>) wurde.</p></div>
|
||||
|
||||
|
||||
<div id="c12572" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Diagenese:</h3><p>Prozess der Verfestigung von <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> zu <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a> unter niedrigen Drucken und Temperaturen unter 200 °C.</p></div>
|
||||
|
||||
|
||||
<div id="c12763" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Dinosaurier:</h3><p>Die s.g. „Schreckensechsen“ (gr.) waren die größten und schwersten auf dem Land lebenden Wirbeltiere der Erdgeschichte. Sie starben Ende des Erdmittelalters aus.</p></div>
|
||||
|
||||
|
||||
<div id="c12573" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Diorit:</h3><p><a href="glossar-p.html#c12697" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plutonisches</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, welches aus <a href="glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plagioklas</a>, wenig <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a> und gewöhnlich <a href="glossar-h.html#c12622" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Hornblende</a> besteht, oft auch mit <a href="glossar-b.html#c12755" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Biotit</a> oder <a href="glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pyroxen</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12574" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Dolomit:</h3><p><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>name für Kalzium-Magnesium-<a href="glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Karbonat</a> (CaMg(CO<sub>3</sub>)<sub>2</sub>), aber auch <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>name für ein <a href="glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>karbonatisches</a><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a>, welches hauptsächlich aus dem <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a> Dolomit besteht. Entsteht überwiegend während der <a href="glossar-d.html#c12572" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Diagenese</a> durch Dolomitisierung von <a href="glossar-k.html#c12756" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalzit</a> und <a href="../glossar.html#c12556" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Aragonit</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12575" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-30"><h3>Dropstone:</h3><p>Isoliertes <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>fragment in Kies- bis Blockgröße, das aus schmelzenden Gletschern bzw. Eisbergen freigesetzt wurde und in feinkörnigen See- oder Meeres<a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>sedimenten</a> eingelagert ist.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
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<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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<div class="row custom-row" id="pageWrap">
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||||
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||||
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|
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|
||||
<div id="c13156" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
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|
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<div id="c12398" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
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<div id="c12983" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
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font-size: 1.2em;
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#maincontent-title h1.csc-firstHeader {
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font-size: 2.2em !important;
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|
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</style></div>
|
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|
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<div id="c12891" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><b>E</b></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12396" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Eisenglimmer:</h3><p>Schuppige Varietät von Hämatit (Fe<sub>2</sub>O<sub>3</sub>), einem Eisenoxid-<a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12764" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Eisenwurzen:</h3><p>Grenzüberschreitende Bezeichnung für eine Region in Niederösterreich, Oberösterreich und der Steiermark, die durch ihren Reichtum an Holz und Wasserkraft früher Standort von Eisen verarbeitenden Betrieben, vor allem für die Erze der Eisenerzer Alpen, war.</p></div>
|
||||
|
||||
|
||||
<div id="c12580" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Eklogit:</h3><p><a href="glossar-m.html#c12662" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> aus hellgrünem <a href="glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pyroxen</a>, rotem <a href="glossar-g.html#c12612" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Granat</a> und ohne <a href="glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plagioklas</a>, entstanden aus <a href="glossar-b.html#c12562" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>basaltischem</a> Ausgangsmaterial unter sehr hohem Druck und hoher Temperatur (> 1,2 GPa Druck und > 500 °C) in mehr als 40 km Tiefe.</p></div>
|
||||
|
||||
|
||||
<div id="c12581" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Endmoräne:</h3><p>Zumeist wallförmige Akkumulation von Schutt entlang der Gletscherzunge oder -front.</p></div>
|
||||
|
||||
|
||||
<div id="c12582" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Epidot:</h3><p>Gelbgrünliches, <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikatisches</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a> mit Kalzium, Eisen und Aluminium.</p></div>
|
||||
|
||||
|
||||
<div id="c12583" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Erdkruste:</h3><p>Äußere feste Schale der Erde, zusammengesetzt aus <a href="glossar-k.html#c12641" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kontinentaler</a> und <a href="glossar-o.html#c12681" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>ozeanischer Kruste</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12584" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Erdmantel:</h3><p>Schale der Erde zwischen der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> und dem Erdkern. Er besteht im oberen Teil aus <a href="glossar-o.html#c12676" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Olivin</a>, <a href="glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pyroxen</a> und untergeordnet <a href="glossar-g.html#c12612" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Granat</a>. Durch den gegen das Erdinnere ansteigenden Druck ändert sich die mineralogische (<a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>) Zusammensetzung des Erdmantels mit der Tiefe.</p></div>
|
||||
|
||||
|
||||
<div id="c12765" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Erdölmuttergestein:</h3><p>Ein Sedimentgestein, das reich an organischer Substanz ist, aus welcher Erdöl und Erdgas gebildet werden.</p></div>
|
||||
|
||||
|
||||
<div id="c12585" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Erosion:</h3><p>Abtragung von <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen</a> und Böden durch die physikalischen und chemischen Wirkungen von Wasser, Wind, Eis, Sonneneinstrahlung und Wurzeldruck. Der Prozess der Erosion kann in <a href="glossar-v.html#c12752" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Verwitterung</a> und Transport unterteilt werden.</p></div>
|
||||
|
||||
|
||||
<div id="c12586" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Erratischer Block („Findling“):</h3><p>Block aus ortsfremdem Fest<a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gestein</a>, der als <a href="glossar-g.html#c12602" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Geschiebe</a> durch Gletschereis an einen anderen Ort verfrachtet wurde.</p></div>
|
||||
|
||||
|
||||
<div id="c12587" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-20"><h3>Exotischer Block:</h3><p><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>block in einer geologisch fremden Umgebung.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
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||||
</div>
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||||
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||||
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<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
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<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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<script src="../../../../unpkg.com/popper.js%401.16.1/dist/umd/popper.min.js"></script>
|
||||
<script src="../../../../unpkg.com/tooltip.js%401.3.3/dist/umd/tooltip.min.js"></script>
|
||||
|
||||
<!-- <script type="text/javascript" src="https://s3.amazonaws.com/cdn.knightlab.com/libs/timeline/latest/js/storyjs-embed.js"></script>-->
|
||||
<script src="../../../fileadmin/template-rocky/timeline/build/js/storyjs-embed.js"></script>
|
||||
<script src="../../../fileadmin/template-rocky/js/responsive-map.js"></script>
|
||||
<script src="../../../fileadmin/template-rocky/js/script.js"></script>
|
||||
|
||||
<script>
|
||||
$(document).ready(function() {
|
||||
createStoryJS({
|
||||
type: 'timeline',
|
||||
width: '800',
|
||||
height: '600',
|
||||
source: '/fileadmin/template-rocky/timeline/example_json.json',
|
||||
embed_id: 'timeline-embed', //OPTIONAL USE A DIFFERENT DIV ID FOR EMBED
|
||||
});
|
||||
});
|
||||
</script>
|
||||
<link rel="canonical" href="glossar-f.html">
|
||||
</head>
|
||||
<body id="page-757">
|
||||
<div class="container-fluid background">
|
||||
<div class="row-fluid">
|
||||
<div class="col-md-5 logo-container">
|
||||
<a href="../../index.html"><img src="../../../fileadmin/template-rocky/img/logo.jpg" alt="Rocky"></a>
|
||||
</div>
|
||||
<div class="col-md-7">
|
||||
<div class="header-maps">
|
||||
<div class="switch">
|
||||
<a href="#" data-target="landschaften">Landschaften</a> | <a href="#" data-target="bausteine">Bausteine</a>
|
||||
</div>
|
||||
<object id="landschaften" class="landschaften map" data="../../fileadmin/template-rocky/img/Karte_Landschaften.svg" type="image/svg+xml">
|
||||
Ihr Browser kann leider kein SVG darstellen.
|
||||
</object>
|
||||
<object id="bausteine" class="bausteine map" data="../../fileadmin/template-rocky/img/Karte_Bausteine.svg" type="image/svg+xml" style="display:none;">
|
||||
Ihr Browser kann leider kein SVG darstellen.
|
||||
</object>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
<div class="row">
|
||||
<div class="col-md-10">
|
||||
<nav id="mainnav">
|
||||
<ul><li><a href="../../landschaften.html">Landschaften</a><ul class="scndLevel clearfix"><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../../grundlagen.html">Grundlagen</a><ul class="scndLevel clearfix"><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../../bausteine.html">Bausteine</a><ul class="scndLevel clearfix"><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul class="scndLevel clearfix"><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="selected"><a href="../../service.html" class="selected">Service</a><ul class="scndLevel clearfix"><li><a href="../download.html">Download</a></li><li class="selected"><a href="../glossar.html" class="selected">Glossar</a></li></ul></li></ul>
|
||||
|
||||
</nav>
|
||||
<div id="mobile-nav">
|
||||
<ul><li><a href="#">Menü</a><ul><li><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li class="last"><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li class="last"><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li class="last"><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li class="last"><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="last"><a href="../../service.html" class="active">Service</a><ul><li><a href="../download.html">Download</a></li><li class="last"><a href="../glossar.html" class="active">Glossar</a></li></ul></li></ul></li></ul>
|
||||
</div>
|
||||
</div>
|
||||
<div class="col-md-2">
|
||||
<div class="container-right-top clearfix">
|
||||
<div id="language">
|
||||
<ul></ul>
|
||||
</div>
|
||||
<div id="textSizer">
|
||||
<div class="fontSize hidden-sm hidden-xs" id="fontsize">
|
||||
<p>
|
||||
<a href="#nogo" class="">
|
||||
<span class="medium">A</span>
|
||||
</a>
|
||||
<a href="#nogo" class="">
|
||||
<span class="large">A</span>
|
||||
</a>
|
||||
</p>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
<div class="container-right-bottom">
|
||||
<div class="search-container">
|
||||
<!--<form action="index.php?id=803" method="post" id="indexedsearch">
|
||||
<input type="hidden" name="tx_indexedsearch[sections]" value="0">
|
||||
<input name="tx_indexedsearch[submit_button]" value="Search" type="hidden">
|
||||
<input name="tx_indexedsearch[sword]" placeholder="Suchbegriff" id="search-field" type="text">
|
||||
<input type="image" src="/fileadmin/template-rocky/img/search.png" id="search-button" class="searchButton" alt="Search" title="Search">
|
||||
</form>-->
|
||||
<form method="get" id="form_kesearch_pi1" name="form_kesearch_pi1" action="https://www.geosphere.at/rocky-austria/suche/">
|
||||
<fieldset class="kesearch_searchbox">
|
||||
<!-- <input type="hidden" name="id" value="803"> -->
|
||||
<!-- <input type="text" id="ke_search_sword" name="tx_kesearch_pi1[sword]" value="" placeholder="Suchbegriff" onfocus="if (this.value == 'Suchbegriff') { this.value = ''; }" onblur="if (this.value == '') { this.value = 'Suchbegriff'; }">
|
||||
<input type="image" src="../../../fileadmin/template-rocky/img/search.png" id="search-button" class="searchButton" alt="Search" title="Suche"> -->
|
||||
<input id="kesearchpagenumber" type="hidden" name="tx_kesearch_pi1[page]" value="1">
|
||||
<input id="resetFilters" type="hidden" name="tx_kesearch_pi1[resetFilters]" value="0">
|
||||
<input id="sortByField" type="hidden" name="tx_kesearch_pi1[sortByField]" value="">
|
||||
<input id="sortByDir" type="hidden" name="tx_kesearch_pi1[sortByDir]" value="">
|
||||
</fieldset>
|
||||
</form>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
|
||||
<div class="row custom-row" id="pageWrap">
|
||||
|
||||
<div class="col-md-3 custom-column">
|
||||
<div id="sidebar" class="content">
|
||||
|
||||
<div id="c13157" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
<div class="col-md-9 custom-column">
|
||||
<div id="maincontent-title" class="content">
|
||||
|
||||
<div id="c12404" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
|
||||
|
||||
<div id="c12984" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
|
||||
#start-right h3, #sidebar h3, #sidebar h2 {
|
||||
margin-top: 0;
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
|
||||
}
|
||||
#maincontent h3 {
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
color: #606c65 !Important;
|
||||
}
|
||||
|
||||
#maincontent-title h1.csc-firstHeader {
|
||||
font-size: 2.2em !important;
|
||||
}
|
||||
#maincontent-title h2 {
|
||||
color: #606c65;
|
||||
margin-top: 0;
|
||||
font-size: 1.6em;
|
||||
margin-top: 0;
|
||||
padding-top: 0;
|
||||
}
|
||||
p {
|
||||
margin-top: 0;
|
||||
}
|
||||
</style></div>
|
||||
|
||||
|
||||
<div id="c12892" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><b>F</b></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12402" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Falte:</h3><p>Systematisch gebogene Schichtung oder Schieferung in einem <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>körper.</p></div>
|
||||
|
||||
|
||||
<div id="c12588" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Faltenachse:</h3><p>Gedachte Linie durch die Punkte der größten Krümmung einer verfalteten Fläche (<a href="glossar-f.html#c12402" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Falte</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12589" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Feldspat-Gruppe:</h3><p><a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Silikatische</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a>, die neben Aluminium auch Kalzium, Natrium und Kalium in wechselnder Menge enthalten. Feldspate sind die häufigsten <a href="glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteinsbildenden</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a> in der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c13224" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Fenster:</h3><p>Als <a href="glossar-t.html#c12738" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>tektonisches</a> Fenster bezeichnen <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Geologen</a> eine Öffnung in einer <a href="glossar-t.html#c12738" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>tektonischen</a> Einheit, in welcher die unterlagernde Einheit sichtbar wird.</p></div>
|
||||
|
||||
|
||||
<div id="c12590" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Feuerstein:</h3><p><a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a>reiches, sehr hartes und scharfkantig brechendes <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a>, das entweder aus <a href="glossar-k.html#c12632" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kieseligen</a> Schwammnadeln und <a href="glossar-r.html#c12767" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Radiolarien</a> gebildet wurde oder durch Sammelkristallisation (<a href="glossar-k.html#c12645" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristallin</a>) <a href="glossar-k.html#c12632" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kieseliger</a> Substanz in <a href="glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>karbonatischen</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimenten</a> entstand.</p></div>
|
||||
|
||||
|
||||
<div id="c12591" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Flöz:</h3><p><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>schicht, die wirtschaftlich wichtige Rohstoffe wie beispielsweise Erz, Kohle oder Salz (<a href="glossar-s.html#c12733" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Steinsalz</a>) enthält oder fast zur Gänze aus ihnen besteht.</p></div>
|
||||
|
||||
|
||||
<div id="c12592" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Flussterrasse (<a href="glossar-t.html#c12739" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Terrasse</a>):</h3><p>Erhöht gelegene, ebene Geländeform; entweder durch Aufschüttung und nachfolgendes Einschneiden (Tiefenerosion; <a href="glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erosion</a>) eines Flusses entstandene Akkumulationsterrasse oder durch seitliche Abtragung (Lateralerosion; <a href="glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erosion</a>) eines Fließgewässers entstandene Felsterrasse.</p></div>
|
||||
|
||||
|
||||
<div id="c12593" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Flysch:</h3><p>Charakteristische Abfolgen von <a href="glossar-s.html#c12711" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sandstein</a>, <a href="glossar-t.html#c12746" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Tonstein</a> und <a href="glossar-m.html#c12661" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mergelstein</a>, die sich oftmals wiederholen; aus <a href="glossar-t.html#c12747" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Trübeströmen</a> in der <a href="glossar-t.html#c12741" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Tiefsee</a> abgelagert und durch Überlagerung verfestigt.</p></div>
|
||||
|
||||
|
||||
<div id="c12594" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Foraminiferen:</h3><p>Vorwiegend <a href="glossar-m.html#c12658" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>marine</a> einzellige Lebewesen, zumeist mit gekammertem, sand- oder kalkschaligem Gehäuse.</p></div>
|
||||
|
||||
|
||||
<div id="c12595" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Fossil:</h3><p>Rest, Abdruck oder Spur eines Lebewesens, das vor mehr als 10 000 Jahren gelebt hat.</p></div>
|
||||
|
||||
|
||||
<div id="c12596" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Frostsprengung:</h3><p>Zerlegung von <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen</a> durch die Druckwirkung des Eises in Gesteinshohlräumen (vor allem in Spalten und <a href="glossar-k.html#c12636" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klüften</a>), bedingt durch die Volumenzunahme des Wassers während des Gefriervorganges.</p></div>
|
||||
|
||||
|
||||
<div id="c12766" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-30"><h3>Fusuliniden:</h3><p>Kalkgehäuse tragende, meeresbewohnende Einzeller aus der Gruppe der Groß<a href="glossar-f.html#c12594" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>foraminiferen</a>, die gegen Ende des Paläozoikums ausstarben.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
|
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<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
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<div class="toggle-content">
|
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<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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<div id="timeline-embed"></div>
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<ul><li><a href="#">Menü</a><ul><li><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li class="last"><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li class="last"><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li class="last"><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li class="last"><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="last"><a href="../../service.html" class="active">Service</a><ul><li><a href="../download.html">Download</a></li><li class="last"><a href="../glossar.html" class="active">Glossar</a></li></ul></li></ul></li></ul>
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<span class="medium">A</span>
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<div id="c13158" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
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Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
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</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
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</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
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<div id="c12410" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
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Glossar
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</span></h1><h2 class="">
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Begriffe von A - Z
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</h2></div>
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<div id="c12893" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><b>G</b></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12408" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Gabbro:</h3><p><a href="glossar-p.html#c12697" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plutonisches</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, welches sich aus <a href="glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plagioklas</a> und <a href="glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pyroxen</a> zusammensetzt. Bei erheblicher Anwesenheit von <a href="glossar-o.html#c12676" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Olivin</a> spricht man von <a href="glossar-o.html#c12676" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Olivin</a>-Gabbro.</p></div>
|
||||
|
||||
|
||||
<div id="c12597" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Ganggestein:</h3><p>In eine Spalte („Gang“) eingedrungene und kristallisierte (<a href="glossar-k.html#c12645" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristallin</a>) Gesteinsschmelze (<a href="glossar-m.html#c12438" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magma</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12598" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Gebirgsbildung:</h3><p>Entstehung eines Gebirges, hauptsächlich durch Prozesse der <a href="glossar-p.html#c12695" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plattentektonik</a> verursacht.</p></div>
|
||||
|
||||
|
||||
<div id="c12599" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Gefügekunde:</h3><p>Lehre von der Analyse und Interpretation der räumlichen Anordnung der <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>bestandteile sowie der definierbaren Raumelemente wie <a href="glossar-k.html#c12636" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klüfte</a>, Schieferungsflächen (<a href="glossar-s.html#c12719" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a>) usw. in einem <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>körper.</p></div>
|
||||
|
||||
|
||||
<div id="c12600" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Geochronologie:</h3><p>Wissenschaftszweig, der die Ereignisse der Erdgeschichte zeitlich absolut datiert; dies geschieht mit Hilfe physikalischer Methoden, z. B. der Messung des Zerfalls von natürlichen radioaktiven Isotopen (<a href="glossar-r.html#c12704" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Radiometrische Altersbestimmung</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12601" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Geologie:</h3><p>Wissenschaft von den dynamischen Prozessen der Erde und deren Entwicklungsgeschichte sowie von den <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen</a> die sie aufbauen und den physikalischen, chemischen und biologischen Veränderungen der Erde.</p></div>
|
||||
|
||||
|
||||
<div id="c13187" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Geomorphologie:</h3><p>Die Geomorphologie oder Landformenkunde ist ein Teilgebiet der Physischen Geographie und untersucht die Formen und form-bildenden Prozesse der Oberfläche der Erde.</p></div>
|
||||
|
||||
|
||||
<div id="c12602" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Geschiebe:</h3><p>Vom Eis bewegte, größere <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>stücke, die beim Eistransport einer charakteristischen Oberflächenbearbeitung unterliegen. Wenn Geschiebe Ritzer und Schrammen aufweisen, werden sie als „gekritzte Geschiebe“ bezeichnet. </p></div>
|
||||
|
||||
|
||||
<div id="c12603" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Gestein:</h3><p>Heterogenes, vielkörniges <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>aggregat, relativ selten auch natürliches Glas oder Rückstand von Organismen. Gesteine treten in selbstständigen, zusammenhängenden, <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>geologisch</a> kartierbaren Körpern auf.</p></div>
|
||||
|
||||
|
||||
<div id="c12604" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Gesteinsbildend:</h3><p>Bezogen auf <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a>, die in genügender Menge und Häufi gkeit vorhanden sind, um <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteine</a> zu bilden. Die wichtigsten sind <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Silikate</a>, <a href="glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Karbonate</a> und Oxide.</p></div>
|
||||
|
||||
|
||||
<div id="c12605" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Gips:</h3><p>Kalziumsulfat (CaSO<sub>4</sub> ⋅ 2 H<sub>2</sub>O); weiß oder rötlich gefärbtes <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a> mit geringer Härte, in <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgesteinen</a> auch <a href="glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteinsbildend</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12606" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Glazial:</h3><p>Klimatisch eine Kaltzeit; geomorphologisch vom Eis geschaffen, auf Gletscher oder Eisschilde bezogen.</p></div>
|
||||
|
||||
|
||||
<div id="c12607" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Glimmer:</h3><p><a href="glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinsbildende </a>Schicht<a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikate</a> mit blättchenförmiger <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristall</a>form. Die wichtigsten Vertreter sind <a href="glossar-b.html#c12755" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Biotit</a> und <a href="glossar-m.html#c12675" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Muskovit</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12608" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Glimmerschiefer:</h3><p>Verbreitetes <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> mit schiefrigem (<a href="glossar-s.html#c12717" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a>) Bruch mit <a href="glossar-g.html#c12607" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Glimmer</a> als einzigem Hauptbestandteil und untergeordnet <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a> und <a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Feldspat</a>. Bei größerem Gehalt an <a href="glossar-g.html#c12612" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Granat</a> spricht man von Granatglimmerschiefer.</p></div>
|
||||
|
||||
|
||||
<div id="c12609" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Gneis:</h3><p>Verbreitetes <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorphes</a> Gestein mit plattigem Bruch. Typisch ist ein Lagenbau, dessen Hauptbestandteile <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a> und <a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Feldspat</a> sind, wobei > 20 % Feldspat und < 50 % <a href="glossar-g.html#c12607" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Glimmer</a> die Zusammensetzungsgrenze zu <a href="glossar-s.html#c12717" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a> markieren.</p></div>
|
||||
|
||||
|
||||
<div id="c12610" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Gondwana:</h3><p>Paläozoischer Großkontinent, in dem die alten Kerne der heutigen Kontinente Südamerika, Afrika, Indien, Australien und Antarktis vereinigt waren. Auch <a href="glossar-b.html#c12378" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Baltica</a> war Teil Gondwanas.</p></div>
|
||||
|
||||
|
||||
<div id="c12611" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Gosau-Gruppe:</h3><p><a href="glossar-s.html#c13189" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schichtfolge</a>, benannt nach der Ortschaft Gosau (O.Ö.), mit großteils <a href="glossar-m.html#c12658" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>marinen</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimenten</a> aus der späten Kreide bis ins Paläogen. Diese wurde während der <a href="../glossar.html#c12549" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Alpidischen Gebirgsbildung</a> zwischen zwei Hauptphasen der <a href="glossar-u.html#c12486" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Überschiebung</a> von <a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Decken</a> abgelagert.</p></div>
|
||||
|
||||
|
||||
<div id="c12612" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Granat-Gruppe:</h3><p>Rötlich gefärbte <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikatische</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a> mit annähernd kugelförmiger <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristallform</a>; <a href="glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteinsbildend</a> in <a href="glossar-g.html#c12608" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Glimmerschiefer</a> und <a href="glossar-g.html#c12609" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gneis</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12613" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Granit:</h3><p><a href="glossar-p.html#c12697" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plutonisches Gestein</a>, welches aus <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a>, Alkali<a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>feldspat</a> und <a href="glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plagioklas</a> besteht, gewöhnlich mit <a href="glossar-b.html#c12755" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Biotit</a> und teilweise auch <a href="glossar-h.html#c12622" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Hornblende</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12614" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Granitgneis:</h3><p><a href="glossar-o.html#c12679" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Orthogneis</a>, dessen Ausgangs<a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gestein</a> als <a href="glossar-g.html#c12613" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Granit</a> identifi ziert werden kann.</p></div>
|
||||
|
||||
|
||||
<div id="c12615" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Granulit:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, das unter sehr hohen Temperaturbedingungen bei 700 – 1 000 °C und 0,4 – 1,8 GPa Druck gebildet wurde. Granulit enthält kaum noch <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a>, die Wasser in der <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristall</a>struktur gebunden haben.</p></div>
|
||||
|
||||
|
||||
<div id="c12616" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Graphit:</h3><p>Kohlenstoff-<a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>, <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorph</a> aus organischen <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimenten</a> oder magmatisch (<a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatit</a>) gebildet.</p></div>
|
||||
|
||||
|
||||
<div id="c12617" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Graphitschiefer:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, dessen Hauptbestandteil <a href="glossar-g.html#c12616" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Graphit</a> ist und dessen parallele Anordnung dem <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> die Schieferung (<a href="glossar-s.html#c12717" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a>) verleiht.</p></div>
|
||||
|
||||
|
||||
<div id="c12618" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Grauwacke:</h3><p>Dunkler, meist grauer oder grünlicher <a href="glossar-s.html#c12711" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sandstein</a> mit toniger (<a href="glossar-t.html#c12743" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ton</a>) Matrix. Bei den <a href="glossar-s.html#c12474" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sand</a>komponenten überwiegt <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a> gegenüber häufi gen <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>bruchstücken.</p></div>
|
||||
|
||||
|
||||
<div id="c12619" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Grundmoräne:</h3><p>An der Basis des Gletschereises gebildete Ablagerung, die sehr dicht gelagert ist und großteils aus feinkörnig zerriebenem <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>material mit einzelnen gröberen Komponenten (<a href="glossar-g.html#c12602" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Geschiebe</a>) besteht.</p></div>
|
||||
|
||||
|
||||
<div id="c12620" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Grünschiefer:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, dessen grünliche Farbe sich von <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineralen</a> wie <a href="../glossar.html#c12552" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Amphibol</a>, <a href="glossar-c.html#c12571" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Chlorit</a> und <a href="glossar-e.html#c12582" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Epidot</a> ableitet und schiefrig (<a href="glossar-s.html#c12717" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a>) bricht; meist hervorgegangen aus <a href="glossar-b.html#c12563" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>basischem</a><a href="glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>vulkanischem</a> Ausgangsmaterial.</p></div>
|
||||
|
||||
|
||||
<div id="c12621" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-100"><h3>Grünschieferfazies:</h3><p>Bedingungen der niedriggradigen <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphose</a> zwischen 300 – 450 °C und 0,1 – 0,8 GPa Druck.</p></div>
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<div class="toggle-button">» Erdgeschichte</div>
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<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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<span class="medium">A</span>
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<span class="large">A</span>
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<form method="get" id="form_kesearch_pi1" name="form_kesearch_pi1" action="https://www.geosphere.at/rocky-austria/suche/">
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</div>
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||||
<div id="c13159" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
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||||
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||||
<div id="c12416" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
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<div id="c12986" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
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#start-right h3, #sidebar h3, #sidebar h2 {
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margin-top: 0;
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font-size: 1.2em;
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font-weight:normal;
|
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|
||||
}
|
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#maincontent h3 {
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
color: #606c65 !Important;
|
||||
}
|
||||
|
||||
#maincontent-title h1.csc-firstHeader {
|
||||
font-size: 2.2em !important;
|
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}
|
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|
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color: #606c65;
|
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margin-top: 0;
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font-size: 1.6em;
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margin-top: 0;
|
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padding-top: 0;
|
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|
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p {
|
||||
margin-top: 0;
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}
|
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</style></div>
|
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<div id="c12894" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><b>H</b></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12414" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Hochgebirge:</h3><p>Gebirge mit hohem Relief, maximalen Höhen über 1 800 m und spitzen Bergformen.</p></div>
|
||||
|
||||
|
||||
<div id="c12977" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Hochquellenwasserleitung:</h3><p>Der Wasserbedarf Wiens wird zu 98% mit der Ersten (135 km) und Zweiten (181 km) Wiener Hochquellenwasserleitung gedeckt. Sie gelten als kulturtechnische Großleistung und bringen hochwertiges Quellwasser aus den Nördlichen Kalkalpen in die Hauptstadt.</p></div>
|
||||
|
||||
|
||||
<div id="c12622" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-60"><h3>Hornblende:</h3><p><a href="glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinsbildendes</a>, dunkelgrünes bis schwarzes, <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikatisches</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a> aus der <a href="../glossar.html#c12552" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Amphibol-Gruppe</a> mit häufig stängeliger <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristall</a>form.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
||||
<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
|
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<div id="timeline-embed"></div>
|
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</div>
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|
||||
<div id="c13160" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
|
||||
|
||||
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|
||||
</div>
|
||||
<div class="col-md-9 custom-column">
|
||||
<div id="maincontent-title" class="content">
|
||||
|
||||
<div id="c12422" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
|
||||
|
||||
<div id="c12987" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
|
||||
#start-right h3, #sidebar h3, #sidebar h2 {
|
||||
margin-top: 0;
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
|
||||
}
|
||||
#maincontent h3 {
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
color: #606c65 !Important;
|
||||
}
|
||||
|
||||
#maincontent-title h1.csc-firstHeader {
|
||||
font-size: 2.2em !important;
|
||||
}
|
||||
#maincontent-title h2 {
|
||||
color: #606c65;
|
||||
margin-top: 0;
|
||||
font-size: 1.6em;
|
||||
margin-top: 0;
|
||||
padding-top: 0;
|
||||
}
|
||||
p {
|
||||
margin-top: 0;
|
||||
}
|
||||
</style></div>
|
||||
|
||||
|
||||
<div id="c12895" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><b>I</b></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c13230" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Impakt:</h3><p>Bezeichnung für den Einschlag eines Meteoriten oder Kometen auf der Erde.</p></div>
|
||||
|
||||
|
||||
<div id="c12420" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Intermediäres Gestein:</h3><p><a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatisches</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> mit einem SiO<sub>2</sub>-Gehalt von 52 – 63 %.</p></div>
|
||||
|
||||
|
||||
<div id="c13231" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-100"><h3>Isostasie:</h3><p>Bezeichnung für das Schwimmgleichgewicht eines festen Körpers in einem plastischen Medium. Im <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>geologische</a>n Zusammenhang bewirkt die Isostasie vertikale Bewegungen innerhalb der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> und zwischen <a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphäre</a> und <a href="../glossar.html#c12557" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Asthenospäre</a>.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
||||
<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
|
||||
<div id="timeline-embed"></div>
|
||||
</div>
|
||||
</div>
|
||||
|
||||
<div class="container-fluid footer">
|
||||
<div class="row footer-menu" id="footer">
|
||||
<ul><li class="first col-md-2 col-sm-12"><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="first col-md-2 col-sm-12"><a href="../../service.html">Service</a><ul><li><a href="../download.html">Download</a></li><li><a href="../glossar.html">Glossar</a></li></ul></li></ul>
|
||||
|
||||
</div>
|
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|
||||
<div class="row">
|
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<div class="col-md-4 gba">
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<a href="https://www.geosphere.at/" target="_blank" title="GeoSphere Austria Standort Neulinggasse">
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<img alt="Link zu www.geologie.ac.at" src="../.././fileadmin/template-rocky/img/logo.013b0f3d.svg" width="160">
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</a>
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</div>
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<div class="col-md-8 text-right">
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<nav id="sitemap">
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<ul><li><a href="../../footer/kontakt.html">Kontakt</a></li><li><a href="https://www.geosphere.at/de/impressum">Impressum</a></li><li><a href="https://www.geosphere.at/de/legal">Datenschutz</a></li><li><a href="../../footer/sitemap.html">Sitemap</a></li></ul>
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</nav>
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</div>
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</div>
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</div>
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<script src="../../../typo3conf/ext/jn_lighterbox/Resources/Public/javascript/lightbox.minea22.js?1646230373"></script>
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<script src="../../../typo3conf/ext/gba/Resources/Public/JavaScript/Dist/scripts10b5.js?1641802928"></script>
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<script>
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/*<![CDATA[*/
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/*TS_inlineFooter*/
|
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lightbox.option({maxHeight:600,showImageNumberLabel:false,});
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/*]]>*/
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</script>
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<script>
|
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|
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$(document).ready(function(){
|
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$('.ce-gallery a.lightbox').each(function(){$(this).attr('title',$(this).attr('data-title'))})
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</body>
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</html>
|
||||
352
rocky-austria/service/glossar/glossar-k.html
Normal file
352
rocky-austria/service/glossar/glossar-k.html
Normal file
|
|
@ -0,0 +1,352 @@
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<!DOCTYPE html>
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||||
<html lang="de-DE">
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<meta charset="utf-8">
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<!--
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{$config.headerComment}
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This website is powered by TYPO3 - inspiring people to share!
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TYPO3 is a free open source Content Management Framework initially created by Kasper Skaarhoj and licensed under GNU/GPL.
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Information and contribution at https://typo3.org/
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-->
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||||
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<base >
|
||||
<link rel="icon" href="https://www.geosphere.at/favicon.ico" type="image/vnd.microsoft.icon">
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<title>Glossar K: Rocky Austria</title>
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<meta http-equiv="x-ua-compatible" content="{$page.meta.compatible}">
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<meta name="generator" content="TYPO3 CMS">
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<meta name="description" content="{$page.meta.description}">
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<meta name="author" content="{$page.meta.author}">
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<meta name="keywords" content="{$page.meta.keywords}">
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<meta name="viewport" content="{$page.meta.viewport}">
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<meta name="robots" content="{$page.meta.robots}">
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<meta property="og:title" content="Glossar K">
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<meta name="twitter:card" content="summary">
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<meta name="apple-mobile-web-app-capable" content="{$page.meta.apple-mobile-web-app-capable}">
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<link rel="stylesheet" href="../../../typo3temp/assets/css/5ca3b44527a764398332ad2c78342db43fac.css?1648457351" media="all">
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<link rel="stylesheet" href="../../../typo3conf/ext/jn_lighterbox/Resources/Public/style/lightbox.minea22.css?1646230373" media="screen">
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<link rel="stylesheet" href="../../../typo3conf/ext/gba/Resources/Public/Css/layout.minc071.css?1647252837" media="all">
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<meta name="viewport" content="width=device-width, initial-scale=1, maximum-scale=1"> <meta http-equiv="X-UA-Compatible" content="IE=edge, chrome=1">
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<meta name="viewport" content="width=device-width, minimum-scale=1.0, maximum-scale=1.0">
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<link href="../../../fileadmin/template-rocky/css/bootstrap.min.css" rel="stylesheet">
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<link href="../../../fileadmin/template-rocky/css/jquery.fancybox.css" rel="stylesheet">
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<link href="../../../fileadmin/template-rocky/js/helpers/jquery.fancybox-buttons.css" rel="stylesheet">
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<link href="../../../fileadmin/template-rocky/css/style.min.css" rel="stylesheet">
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<link rel="stylesheet" href="../../../../use.fontawesome.com/releases/v5.0.13/css/all.css" integrity="sha384-DNOHZ68U8hZfKXOrtjWvjxusGo9WQnrNx2sqG0tfsghAvtVlRW3tvkXWZh58N9jp" crossorigin="anonymous">
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<link href="https://www.geosphere.at/fileadmin/template-rocky/img/favicon.ico" rel="icon" type="image/x-icon">
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<!--[if lt IE 9]>
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<script src="http://html5shiv.googlecode.com/svn/trunk/html5.js"></script>
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<![endif]-->
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<script src="../../../fileadmin/template-rocky/js/jquery-1.11.1.min.js"></script>
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<script src="../../../fileadmin/template-rocky/js/jquery.fancybox.pack.js"></script>
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<script type="text/javascript" src="../../../fileadmin/template/js/jquery.textresizer.min.js"></script>
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<script src="../../../fileadmin/template-rocky/js/helpers/jquery.fancybox-buttons.js"></script>
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<script src="../../../../unpkg.com/popper.js%401.16.1/dist/umd/popper.min.js"></script>
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<script src="../../../../unpkg.com/tooltip.js%401.3.3/dist/umd/tooltip.min.js"></script>
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<!-- <script type="text/javascript" src="https://s3.amazonaws.com/cdn.knightlab.com/libs/timeline/latest/js/storyjs-embed.js"></script>-->
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<script src="../../../fileadmin/template-rocky/timeline/build/js/storyjs-embed.js"></script>
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<script src="../../../fileadmin/template-rocky/js/responsive-map.js"></script>
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<script src="../../../fileadmin/template-rocky/js/script.js"></script>
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<script>
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||||
$(document).ready(function() {
|
||||
createStoryJS({
|
||||
type: 'timeline',
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||||
width: '800',
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||||
height: '600',
|
||||
source: '/fileadmin/template-rocky/timeline/example_json.json',
|
||||
embed_id: 'timeline-embed', //OPTIONAL USE A DIFFERENT DIV ID FOR EMBED
|
||||
});
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});
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<link rel="canonical" href="glossar-k.html">
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</head>
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<body id="page-761">
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<div class="row-fluid">
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||||
<a href="../../index.html"><img src="../../../fileadmin/template-rocky/img/logo.jpg" alt="Rocky"></a>
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</div>
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<div class="col-md-7">
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<div class="header-maps">
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<div class="switch">
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<a href="#" data-target="landschaften">Landschaften</a> | <a href="#" data-target="bausteine">Bausteine</a>
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</div>
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<object id="landschaften" class="landschaften map" data="../../fileadmin/template-rocky/img/Karte_Landschaften.svg" type="image/svg+xml">
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Ihr Browser kann leider kein SVG darstellen.
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</object>
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<object id="bausteine" class="bausteine map" data="../../fileadmin/template-rocky/img/Karte_Bausteine.svg" type="image/svg+xml" style="display:none;">
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Ihr Browser kann leider kein SVG darstellen.
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</object>
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<div class="row">
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<div class="col-md-10">
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<nav id="mainnav">
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<div id="c13161" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
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||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
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<div id="c12428" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
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||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
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font-weight:normal;
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color: #606c65 !Important;
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#maincontent-title h1.csc-firstHeader {
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<div id="c12896" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><b>K</b></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12426" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kaledonische Gebirgsbildung:</h3><p>Entstehung der frühpaläozoischen Gebirge Nordeuropas, benannt nach dem lateinisch-keltischen Namen für Schottland („Caledonia“).</p></div>
|
||||
|
||||
|
||||
<div id="c12623" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kalk(stein):</h3><p><a href="glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Karbonatisches</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> bzw. <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a>, welches überwiegend aus <a href="glossar-k.html#c12756" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalzit</a> besteht.</p></div>
|
||||
|
||||
|
||||
<div id="c12624" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kalkglimmerschiefer:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorpher</a><a href="glossar-g.html#c12607" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>glimmerreicher</a><a href="glossar-s.html#c12717" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a> mit <a href="glossar-t.html#c12743" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>tonig</a>-<a href="glossar-s.html#c12474" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>sandig</a>-<a href="glossar-k.html#c12623" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kalkigem</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> als Ausgangsmaterial.</p></div>
|
||||
|
||||
|
||||
<div id="c12625" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kalkschiefer:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorpher</a><a href="glossar-s.html#c12717" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a>, der als Hauptbestandteil <a href="glossar-k.html#c12756" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalzit</a> enthält und aus <a href="glossar-k.html#c12623" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kalkig</a>-<a href="glossar-t.html#c12743" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>tonigem</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> hervorgegangen ist.</p></div>
|
||||
|
||||
|
||||
<div id="c12626" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kältesteppe:</h3><p>Baumlose Landschaft mit verbreitet Dauerfrostboden (Synonym für Tundra).</p></div>
|
||||
|
||||
|
||||
<div id="c12756" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kalzit:</h3><p><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>name für Kalziumkarbonat (CaCO<sub>3</sub>); häufig <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteins</a>bildend.</p></div>
|
||||
|
||||
|
||||
<div id="c12627" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kaolin:</h3><p>Hauptsächlich aus Kaolinit (Aluminiumhydro<a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikat</a>) aufgebauter, weißlicher <a href="glossar-t.html#c12743" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ton</a>; Rohstoff für die Keramik- und Papierindustrie.</p></div>
|
||||
|
||||
|
||||
<div id="c12628" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kar:</h3><p>Durch <a href="glossar-g.html#c12606" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>glaziale</a><a href="glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erosion</a> entstandene halbrunde Hohlform in Bergflanken.</p></div>
|
||||
|
||||
|
||||
<div id="c13228" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Karbon:</h3><p>Abschnitt im Erdalterum (Paläozoikum) basierend auf den zahlreichen Steinkohlelagerstätten aus dieser Periode (früher auch Steinkohlezeit).</p></div>
|
||||
|
||||
|
||||
<div id="c12629" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Karbonat:</h3><p>Salz der Kohlensäure; <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>geologisch</a> bedeutend sind die beiden <a href="glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteinsbildenden</a> Karbonat-<a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a><a href="glossar-k.html#c12756" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalzit</a> und <a href="glossar-d.html#c12574" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Dolomit</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12630" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Karst:</h3><p>Unter- und oberirdische Geländeformen in <a href="glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Karbonatgesteinen</a> (zum Teil auch in Sulfat- und Salz<a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteinen</a>), die vorwiegend durch Kohlensäure<a href="glossar-v.html#c12752" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>verwitterung</a> (oder Lösungs<a href="glossar-v.html#c12752" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>verwitterung</a>) sowie Ausfällung von <a href="glossar-k.html#c12623" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalksteinen</a> und ähnlichen <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgesteinen</a> mit hohen Gehalten an <a href="glossar-k.html#c12756" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalzit</a> entstanden sind.
|
||||
</p><p>Hauptmerkmal ist der überwiegend unterirdische Wasserhaushalt, der nicht auf einer primären Porosität des <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a> beruht, sondern vielmehr sekundär durch den in <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>geologischen</a> Zeiträumen stattfindenden Prozess der Verkarstung (d.h. Korrosion) bedingt ist.</p></div>
|
||||
|
||||
|
||||
<div id="c12631" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kies:</h3><p>Grobkörniges (Körnung zwischen 2 und 63 mm) <a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>klastisches</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> mit überwiegend gerundeten Komponenten (<a href="glossar-s.html#c12721" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schotter</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12632" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kieselig:</h3><p>Reich an <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12633" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kieseliger Schiefer:</h3><p><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a> aus <a href="glossar-t.html#c12743" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ton</a> und einem hohen Anteil an feinstkörnigem <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a>, der aus Skeletten von <a href="glossar-r.html#c12767" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Radiolarien</a> (<a href="glossar-r.html#c12468" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Radiolarit</a>) stammt.</p></div>
|
||||
|
||||
|
||||
<div id="c12634" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kieselsäuren:</h3><p>Sauerstoffsäuren des Siliziums. Als Summenformel wird häufi g SiO<sub>2</sub> ⋅ n H<sub>2</sub>O angegeben; das Wasser ist bei Kieselsäuren jedoch kein <a href="glossar-k.html#c12645" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristall</a>wasser, sondern kann nur durch eine chemische Reaktion abgespalten werden. Formales Endprodukt der Wasserabspaltung ist Siliziumdioxid (SiO2; <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a>). Die Salze der Kieselsäuren nennt man <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Silikate</a>; kieselsäurereiche <a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>magmatische Gesteine</a> werden als „sauer“ bezeichnet (<a href="glossar-s.html#c12712" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>saures Gestein</a>), kieselsäurearme als „basisch“ (<a href="glossar-b.html#c12563" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>basisches Gestein</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12757" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Klastisch:</h3><p>Bezeichnung für aus festen Bruchstücken bestehendes <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> oder <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a>, welches durch mechanische <a href="glossar-v.html#c12752" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Verwitterung</a> von <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen</a> und deren nachfolgenden Transport entstanden ist.</p></div>
|
||||
|
||||
|
||||
<div id="c13234" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Klimaarchive:</h3><p>In Moor- und Seeablagerungen finden sich meist reichlich <a href="glossar-f.html#c12595" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>fossile</a> Pollen und Sporen, die zur Rekonstruktion der früheren Pflanzengemeinschaften – und damit indirekt des Klimas – verwendet werden.</p></div>
|
||||
|
||||
|
||||
<div id="c12635" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Klippe:</h3><p>Relativ kleiner Teil einer <a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Decke</a>, der durch <a href="glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erosion</a> vom Hauptkörper abgetrennt ist.</p></div>
|
||||
|
||||
|
||||
<div id="c12636" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kluft:</h3><p>Ebener Bruch oder Riss in einem <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> ohne seitliche Versetzung, entstanden durch diagenetische (<a href="glossar-d.html#c12572" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Diagenese</a>) Prozesse, tektonische (<a href="glossar-t.html#c12737" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Tektonik</a>) Beanspruchung oder Abkühlung. Die Größenordnung einer geöffneten Kluft liegt im Bereich von wenigen Millimetern Weite bis zu einer Erstreckung von mehreren Metern.</p></div>
|
||||
|
||||
|
||||
<div id="c12637" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kluftkörper:</h3><p><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>körper, der allseitig von <a href="glossar-k.html#c12636" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klüften</a> begrenzt wird.</p></div>
|
||||
|
||||
|
||||
<div id="c12638" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kohlenwasserstoffe:</h3><p>Chemische Verbindungen aus Kohlenstoff und Wasserstoff; <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>geologisch</a> und wirtschaftlich bedeutend sind sie als Hauptbestandteile von Erdöl- und Erdgaslagerstätten, gebildet im Laufe von Jahrmillionen aus organischem Material unter reduzierenden Bedingungen in einer Tiefe zwischen 2 000 und 6 000 m.</p></div>
|
||||
|
||||
|
||||
<div id="c12639" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Konglomerat:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klastisches</a><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a> mit mindestens 50 % gerundeten Komponenten (Körnung größer 2 mm); verfestigter <a href="glossar-k.html#c12631" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kies</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12640" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Konkordanz:</h3><p>Ungestörte und gleichlaufende (konkordante) Überlagerung von älteren durch jüngere <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>schichten; Hinweis auf durchgehende Ablagerung (<a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12641" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kontinentale Kruste:</h3><p>Jener Teil der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a>, der aus relativ leichtem Material besteht, mit überwiegend <a href="glossar-s.html#c12712" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>sauren Gesteinen</a> wie <a href="glossar-g.html#c12613" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Granit</a>, <a href="glossar-g.html#c12609" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gneis</a> und <a href="glossar-s.html#c12717" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a> und in größerer Tiefe auch <a href="glossar-b.html#c12563" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>basischen Gesteinen</a> wie <a href="glossar-d.html#c12573" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Diorit</a> und <a href="glossar-g.html#c12408" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gabbro</a>. Aus ihr sind die Kontinente mitsamt ihren <a href="glossar-s.html#c12713" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schelf</a>gebieten und dem <a href="glossar-k.html#c12642" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kontinentalhang</a> aufgebaut.</p></div>
|
||||
|
||||
|
||||
<div id="c12642" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kontinentalhang:</h3><p>Sub<a href="glossar-m.html#c12658" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>mariner</a> Hangbereich zwischen <a href="glossar-s.html#c12713" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schelf</a> und <a href="glossar-t.html#c12741" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Tiefsee</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12643" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Konvektionsströmungen:</h3><p>Sehr langsame Fließbewegungen im <a href="glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdmantel</a>, verursacht durch Temperatur und Dichteunterschiede, die durch den Wärmefluss aus dem Erdinneren entstehen. Gelten als wesentliche Ursache der Bewegung der <a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphären</a>platten (<a href="glossar-p.html#c12695" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plattentektonik</a>).</p></div>
|
||||
|
||||
|
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<div id="c12867" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kraton:</h3><p>Sehr alter Kernbereich eines Kontinents, der durch paläozoische oder spätere <a href="glossar-g.html#c12598" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gebirgsbildungen</a> nicht mehr verformt wurde.</p></div>
|
||||
|
||||
|
||||
<div id="c12644" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Kristall:</h3><p>Festkörper, dessen Atome oder Moleküle in einem dreidimensionalen Kristallgitter regelmäßig angeordnet sind.</p></div>
|
||||
|
||||
|
||||
<div id="c12645" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-180"><h3>Kristallin:</h3><p>Bezeichnung für <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kristall</a>isiertes Material, in der <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Geologie</a> für <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteine</a> und <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a>; <a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>magmatische</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteine</a><a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kristall</a>isieren aus einer <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>schmelze (<a href="glossar-m.html#c12438" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magma</a>), während <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorphe</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteine</a> in festem Zustand neu <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kristall</a>isieren (<a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphose</a>).</p></div>
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||||
/*<![CDATA[*/
|
||||
/*TS_inlineFooter*/
|
||||
lightbox.option({maxHeight:600,showImageNumberLabel:false,});
|
||||
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||||
/*]]>*/
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||||
</script>
|
||||
<script>
|
||||
|
||||
$(document).ready(function(){
|
||||
$('.ce-gallery a.lightbox').each(function(){$(this).attr('title',$(this).attr('data-title'))})
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|
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</html>
|
||||
294
rocky-austria/service/glossar/glossar-l.html
Normal file
294
rocky-austria/service/glossar/glossar-l.html
Normal file
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@ -0,0 +1,294 @@
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|||
<!DOCTYPE html>
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<html lang="de-DE">
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<base >
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<link rel="stylesheet" href="../../../../use.fontawesome.com/releases/v5.0.13/css/all.css" integrity="sha384-DNOHZ68U8hZfKXOrtjWvjxusGo9WQnrNx2sqG0tfsghAvtVlRW3tvkXWZh58N9jp" crossorigin="anonymous">
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<script>
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$(document).ready(function() {
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createStoryJS({
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||||
type: 'timeline',
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width: '800',
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||||
height: '600',
|
||||
source: '/fileadmin/template-rocky/timeline/example_json.json',
|
||||
embed_id: 'timeline-embed', //OPTIONAL USE A DIFFERENT DIV ID FOR EMBED
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||||
});
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||||
});
|
||||
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<link rel="canonical" href="glossar-l.html">
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<a href="../../index.html"><img src="../../../fileadmin/template-rocky/img/logo.jpg" alt="Rocky"></a>
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</div>
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<div class="col-md-7">
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<div class="header-maps">
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<div class="switch">
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<a href="#" data-target="landschaften">Landschaften</a> | <a href="#" data-target="bausteine">Bausteine</a>
|
||||
</div>
|
||||
<object id="landschaften" class="landschaften map" data="../../fileadmin/template-rocky/img/Karte_Landschaften.svg" type="image/svg+xml">
|
||||
Ihr Browser kann leider kein SVG darstellen.
|
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</object>
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||||
<object id="bausteine" class="bausteine map" data="../../fileadmin/template-rocky/img/Karte_Bausteine.svg" type="image/svg+xml" style="display:none;">
|
||||
Ihr Browser kann leider kein SVG darstellen.
|
||||
</object>
|
||||
</div>
|
||||
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|
||||
</div>
|
||||
<div class="row">
|
||||
<div class="col-md-10">
|
||||
<nav id="mainnav">
|
||||
<ul><li><a href="../../landschaften.html">Landschaften</a><ul class="scndLevel clearfix"><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../../grundlagen.html">Grundlagen</a><ul class="scndLevel clearfix"><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../../bausteine.html">Bausteine</a><ul class="scndLevel clearfix"><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul class="scndLevel clearfix"><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="selected"><a href="../../service.html" class="selected">Service</a><ul class="scndLevel clearfix"><li><a href="../download.html">Download</a></li><li class="selected"><a href="../glossar.html" class="selected">Glossar</a></li></ul></li></ul>
|
||||
|
||||
</nav>
|
||||
<div id="mobile-nav">
|
||||
<ul><li><a href="#">Menü</a><ul><li><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li class="last"><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li class="last"><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li class="last"><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li class="last"><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="last"><a href="../../service.html" class="active">Service</a><ul><li><a href="../download.html">Download</a></li><li class="last"><a href="../glossar.html" class="active">Glossar</a></li></ul></li></ul></li></ul>
|
||||
</div>
|
||||
</div>
|
||||
<div class="col-md-2">
|
||||
<div class="container-right-top clearfix">
|
||||
<div id="language">
|
||||
<ul></ul>
|
||||
</div>
|
||||
<div id="textSizer">
|
||||
<div class="fontSize hidden-sm hidden-xs" id="fontsize">
|
||||
<p>
|
||||
<a href="#nogo" class="">
|
||||
<span class="medium">A</span>
|
||||
</a>
|
||||
<a href="#nogo" class="">
|
||||
<span class="large">A</span>
|
||||
</a>
|
||||
</p>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
<div class="container-right-bottom">
|
||||
<div class="search-container">
|
||||
<!--<form action="index.php?id=803" method="post" id="indexedsearch">
|
||||
<input type="hidden" name="tx_indexedsearch[sections]" value="0">
|
||||
<input name="tx_indexedsearch[submit_button]" value="Search" type="hidden">
|
||||
<input name="tx_indexedsearch[sword]" placeholder="Suchbegriff" id="search-field" type="text">
|
||||
<input type="image" src="/fileadmin/template-rocky/img/search.png" id="search-button" class="searchButton" alt="Search" title="Search">
|
||||
</form>-->
|
||||
<form method="get" id="form_kesearch_pi1" name="form_kesearch_pi1" action="https://www.geosphere.at/rocky-austria/suche/">
|
||||
<fieldset class="kesearch_searchbox">
|
||||
<!-- <input type="hidden" name="id" value="803"> -->
|
||||
<!-- <input type="text" id="ke_search_sword" name="tx_kesearch_pi1[sword]" value="" placeholder="Suchbegriff" onfocus="if (this.value == 'Suchbegriff') { this.value = ''; }" onblur="if (this.value == '') { this.value = 'Suchbegriff'; }">
|
||||
<input type="image" src="../../../fileadmin/template-rocky/img/search.png" id="search-button" class="searchButton" alt="Search" title="Suche"> -->
|
||||
<input id="kesearchpagenumber" type="hidden" name="tx_kesearch_pi1[page]" value="1">
|
||||
<input id="resetFilters" type="hidden" name="tx_kesearch_pi1[resetFilters]" value="0">
|
||||
<input id="sortByField" type="hidden" name="tx_kesearch_pi1[sortByField]" value="">
|
||||
<input id="sortByDir" type="hidden" name="tx_kesearch_pi1[sortByDir]" value="">
|
||||
</fieldset>
|
||||
</form>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
|
||||
<div class="row custom-row" id="pageWrap">
|
||||
|
||||
<div class="col-md-3 custom-column">
|
||||
<div id="sidebar" class="content">
|
||||
|
||||
<div id="c13162" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
<div class="col-md-9 custom-column">
|
||||
<div id="maincontent-title" class="content">
|
||||
|
||||
<div id="c12434" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
|
||||
|
||||
<div id="c12989" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
|
||||
#start-right h3, #sidebar h3, #sidebar h2 {
|
||||
margin-top: 0;
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
|
||||
}
|
||||
#maincontent h3 {
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
color: #606c65 !Important;
|
||||
}
|
||||
|
||||
#maincontent-title h1.csc-firstHeader {
|
||||
font-size: 2.2em !important;
|
||||
}
|
||||
#maincontent-title h2 {
|
||||
color: #606c65;
|
||||
margin-top: 0;
|
||||
font-size: 1.6em;
|
||||
margin-top: 0;
|
||||
padding-top: 0;
|
||||
}
|
||||
p {
|
||||
margin-top: 0;
|
||||
}
|
||||
</style></div>
|
||||
|
||||
|
||||
<div id="c12897" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><b>L</b></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12432" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Lagune:</h3><p>Seichter Meeresbereich, der durch <a href="glossar-s.html#c12474" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sand</a>ablagerungen oder <a href="glossar-r.html#c12707" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Riffe</a> vom offenen Meer abgetrennt ist.</p></div>
|
||||
|
||||
|
||||
<div id="c12646" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Laurasia:</h3><p>Ehemaliger mesozoischer Kontinent, der durch das Auseinanderbrechen von <a href="glossar-p.html#c12683" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pangäa</a> im Jura entstand und in der späten Kreide mit der durchgehenden Öffnung des Nordatlantiks in das heutige Nordamerika und Eurasien zerfiel.</p></div>
|
||||
|
||||
|
||||
<div id="c12647" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Laurentia:</h3><p>Ehemaliger neoproterozoischer bis früh paläozoischer Kontinent, der weite Teile des heutigen Nordamerika sowie Grönland aufbaut.</p></div>
|
||||
|
||||
|
||||
<div id="c12648" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Laurussia:</h3><p>Ehemaliger paläozoischer Kontinent, der im Zuge der <a href="glossar-k.html#c12426" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kaledonischen Gebirgsbildung</a> aus den Kontinenten <a href="glossar-b.html#c12378" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Baltica</a> und <a href="glossar-l.html#c12647" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Laurentia</a> entstand.</p></div>
|
||||
|
||||
|
||||
<div id="c12649" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Lava:</h3><p>Hochtemperierte <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>schmelze (<a href="glossar-m.html#c12438" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magma</a>), die bei vulkanischer Tätigkeit (<a href="glossar-v.html#c12753" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Vulkanismus</a>) an der Erdoberfläche austritt.</p></div>
|
||||
|
||||
|
||||
<div id="c12650" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Leitfossil:</h3><p>Tierisches oder pflanzliches <a href="glossar-f.html#c12595" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Fossil</a>, mit dem sich das relative Alter des umschließenden <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a> ermitteln lässt; ideale Leitfossilien waren möglichst kurzlebig und weit verbreitet.</p></div>
|
||||
|
||||
|
||||
<div id="c12651" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Lithologie:</h3><p>Beschreibung und Unterscheidung von <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen</a> nach äußeren Merkmalen. Häufig wird die mineralische (<a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>) Zusammensetzung und Textur eines Gesteins als dessen Lithologie bezeichnet.</p></div>
|
||||
|
||||
|
||||
<div id="c12652" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Lithosphäre:</h3><p>Umfasst die <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> und den obersten, starren Teil des <a href="glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdmantels</a>; ist in Platten (= Lithosphärenplatten; <a href="glossar-p.html#c12695" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plattentektonik</a>) gegliedert.</p></div>
|
||||
|
||||
|
||||
<div id="c12653" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Lithosphärischer Mantel:</h3><p>Oberster starrer Teil des <a href="glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdmantels</a> (10 – 200 km) mit einer Temperatur von weniger als 1300° C, der den tieferen Teil der <a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphäre</a> aufbaut.</p></div>
|
||||
|
||||
|
||||
<div id="c12654" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-10"><h3>Löss:</h3><p>Windverfrachtetes, feinkörniges, ungeschichtetes <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a>, das während Kaltzeiten (<a href="glossar-g.html#c12606" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Glazial</a>) in nicht vergletscherten Gebieten abgelagert wurde. Typisch ist die durch die <a href="glossar-k.html#c12623" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kalk</a>ige Verkittung gegebene Standfestigkeit (Hohlwege, Weinkeller).</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
||||
<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
|
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<div id="timeline-embed"></div>
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<ul><li class="first col-md-2 col-sm-12"><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="first col-md-2 col-sm-12"><a href="../../service.html">Service</a><ul><li><a href="../download.html">Download</a></li><li><a href="../glossar.html">Glossar</a></li></ul></li></ul>
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<object id="bausteine" class="bausteine map" data="../../fileadmin/template-rocky/img/Karte_Bausteine.svg" type="image/svg+xml" style="display:none;">
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<div id="c13163" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
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||||
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<div id="c12440" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
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||||
</div>
|
||||
<div id="maincontent" class="content">
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<div id="c12990" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
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#start-right h3, #sidebar h3, #sidebar h2 {
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margin-top: 0;
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font-weight:normal;
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}
|
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#maincontent h3 {
|
||||
font-size: 1.2em;
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||||
font-weight:normal;
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color: #606c65 !Important;
|
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}
|
||||
|
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#maincontent-title h1.csc-firstHeader {
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||||
font-size: 2.2em !important;
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}
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#maincontent-title h2 {
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color: #606c65;
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margin-top: 0;
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margin-top: 0;
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}
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</style></div>
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||||
<div id="c12898" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><b>M</b></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12438" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Magma:</h3><p>Hochtemperierte <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>schmelze, Ausgangsmaterial für magmatische <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteine</a> (Erstarrungsgesteine = <a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatite</a>): Tiefengesteine = <a href="glossar-p.html#c12697" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plutonite</a>, Ganggesteine, Ergussgesteine = <a href="glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Vulkanite</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12655" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Magmatit (Erstarrungsgestein):</h3><p>Ein <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, das aus einer Schmelze (<a href="glossar-m.html#c12438" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magma</a>) erstarrt ist.</p></div>
|
||||
|
||||
|
||||
<div id="c12656" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Magmatismus:</h3><p>Zusammenfassender Begriff für alle <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>geologischen</a> Prozesse, an denen <a href="glossar-m.html#c12438" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magma</a> beteiligt ist (<a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatit</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12657" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Magnesit:</h3><p><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>name für Magnesium<a href="glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>karbonat</a> (MgCO<sub>3</sub>); wichtiger Rohstoff für hochfeuerfeste Produkte. </p></div>
|
||||
|
||||
|
||||
<div id="c12658" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Marin:</h3><p>Auf das Meer bezogen.</p></div>
|
||||
|
||||
|
||||
<div id="c12659" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Marmor:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a>, <a href="glossar-k.html#c12645" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kristallines</a><a href="glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Karbonatgestein</a>; technisch wird auch nicht <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorphes</a>, polierbares <a href="glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Karbonatgestein</a> so bezeichnet.</p></div>
|
||||
|
||||
|
||||
<div id="c13235" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Massenbewegungen:</h3><p>Schnelle oder langsame, schwerkraftbedingte Massenverlagerungen von Fest- oder Lockergesteinen von höheren zu tiefer gelegenen Bereichen.</p></div>
|
||||
|
||||
|
||||
<div id="c12660" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Mergel:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klastisches</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> aus <a href="glossar-t.html#c12743" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ton</a> und <a href="glossar-k.html#c12623" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalk</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12661" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Mergelstein:</h3><p>Feinkörniges <a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>klastisches</a><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a> aus <a href="glossar-t.html#c12743" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ton</a> und <a href="glossar-k.html#c12623" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalk</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12662" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Metamorphit:</h3><p>Ein durch <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphose</a> verändertes Gestein.</p></div>
|
||||
|
||||
|
||||
<div id="c12663" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Metamorphose:</h3><p><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>umwandlung im vorwiegend festen Zustand durch Verformung sowie durch Druck- und Temperaturbedingungen, die von den ursprünglichen Bildungsbedingungen abweichen und eine neue <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristall</a>isation hervorrufen.</p></div>
|
||||
|
||||
|
||||
<div id="c12664" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Migmatit:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, welches teilweise aufgeschmolzen wurde und typischerweise aus dunklen und hellen Anteilen besteht. Die dunkleren Teile zeigen Eigenschaften von <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorphen</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen</a>, dagegen zeigen die hellen Teile ein <a href="glossar-m.html#c12656" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>magmatisches</a> (<a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatit</a>) Erscheinungsbild.</p></div>
|
||||
|
||||
|
||||
<div id="c12665" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Mikrofossilien:</h3><p>Kleine (< 2 mm), nur mit optischen Hilfsmitteln (Mikroskop) bestimmbare <a href="glossar-f.html#c12595" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Fossilien</a> wie z. B. <a href="glossar-f.html#c12594" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Foraminiferen</a>, <a href="glossar-r.html#c12767" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Radiolarien</a> (<a href="glossar-r.html#c12468" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Radiolarit</a>), Pollen etc.</p></div>
|
||||
|
||||
|
||||
<div id="c12666" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Mineral:</h3><p>Natürlich gebildeter homogener Festkörper, meist <a href="glossar-k.html#c12645" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kristallin</a> und anorganisch. <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Silikate</a> sind die häufigsten <a href="glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteinsbildenden</a> Minerale.</p></div>
|
||||
|
||||
|
||||
<div id="c12667" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Mittelgebirge:</h3><p>Gebirge mit Höhendifferenzen bis zu 500 m, einer maximalen Höhe von etwa 1 500 bis 1 800 m und rundlichen Formen.</p></div>
|
||||
|
||||
|
||||
<div id="c12668" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Mittelozeanischer Rücken:</h3><p>1 000 – 4 000 km breiter Rücken, der sich vom Tiefseeboden in ca. 5 km Tiefe mit meist sehr geringer Steigung auf ca. 2,5 km Wassertiefe erhebt. An Mittelozeanischen Rücken wird <a href="glossar-o.html#c12681" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>ozeanische Kruste</a> neu gebildet, daher sind sie seismisch sehr aktiv.</p></div>
|
||||
|
||||
|
||||
<div id="c12669" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Mohorovičić-Diskontinuität:</h3><p>Grenze zwischen der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> und dem <a href="glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdmantel</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12670" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Molasse:</h3><p>Abtragungsprodukte eines neu entstandenen Gebirges, die in <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a>becken (Sediment) im Vorland oder auch innerhalb des Gebirgskörpers abgelagert wurden (von frz. „mollasse“: sehr weich).</p></div>
|
||||
|
||||
|
||||
<div id="c12671" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Moldanubikum:</h3><p><a href="glossar-t.html#c12737" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Tektonische</a> Einheit in der <a href="glossar-b.html#c12567" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Böhmischen Masse</a>, benannt nach den Flüssen Moldau und Donau.</p></div>
|
||||
|
||||
|
||||
<div id="c12672" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Moräne:</h3><p><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a>, welches durch Ausschmelzen von mit Gletschern transportiertem <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>schutt entstanden ist. Bildet ein Gemisch aus <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>bruchstücken unterschiedlichster Korngröße und zeigt keine Sortierung oder Schichtung.</p></div>
|
||||
|
||||
|
||||
<div id="c12673" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Moravikum:</h3><p><a href="glossar-t.html#c12738" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Tektonische</a> Einheit in der <a href="glossar-b.html#c12567" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Böhmischen Masse</a>, benannt nach Mähren (tschechisch „Morava“).</p></div>
|
||||
|
||||
|
||||
<div id="c12674" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Mure:</h3><p>Schnell talwärts fließender Strom aus einem Gemisch von Wasser, Feinmaterial und bis zu tonnenschweren Blöcken.</p></div>
|
||||
|
||||
|
||||
<div id="c12675" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-140"><h3>Muskovit:</h3><p>Helles, glänzendes <a href="glossar-g.html#c12607" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Glimmer</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>mineral</a>.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
||||
<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
|
||||
<div id="timeline-embed"></div>
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</div>
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</div>
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<ul><li class="first col-md-2 col-sm-12"><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="first col-md-2 col-sm-12"><a href="../../service.html">Service</a><ul><li><a href="../download.html">Download</a></li><li><a href="../glossar.html">Glossar</a></li></ul></li></ul>
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<div id="c13164" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
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</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
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<div id="c12444" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-5"><h3>Nunatak:</h3><p>Über die Eisoberfläche eines Gletschers aufragender Berg; die Bezeichnung stammt aus dem Grönländischen.</p></div>
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||||
<div id="c13165" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
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<div id="c12452" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
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|
||||
<div id="maincontent" class="content">
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||||
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margin-top: 0;
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font-size: 1.2em;
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||||
font-weight:normal;
|
||||
|
||||
}
|
||||
#maincontent h3 {
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
color: #606c65 !Important;
|
||||
}
|
||||
|
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#maincontent-title h1.csc-firstHeader {
|
||||
font-size: 2.2em !important;
|
||||
}
|
||||
#maincontent-title h2 {
|
||||
color: #606c65;
|
||||
margin-top: 0;
|
||||
font-size: 1.6em;
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margin-top: 0;
|
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padding-top: 0;
|
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p {
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margin-top: 0;
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}
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</style></div>
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|
||||
<div id="c12900" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><b>O</b></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12450" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Obduktion:</h3><p><a href="glossar-u.html#c12486" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Überschiebun</a>g von Decken aus ozeanischer <a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphäre</a> auf eine kontinentale <a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphäre</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12676" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Olivin:</h3><p>Blassgrünes <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikatisches</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a> mit viel Magnesium und weniger Eisen; charakteristisches <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a> in <a href="glossar-b.html#c12563" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>basischen</a><a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatiten</a> der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> und häufigstes <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a> im <a href="glossar-u.html#c12750" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ultrabasit</a> des oberen <a href="glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdmantels</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12677" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Ophiolith:</h3><p>Stück ozeanischer <a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphäre</a>, das durch <a href="glossar-t.html#c12738" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>tektonische</a> Prozesse in die <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> eingebaut wurde. Typisch ist eine <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>abfolge von <a href="glossar-u.html#c12750" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ultrabasit</a> über <a href="glossar-g.html#c12408" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gabbro</a> und <a href="glossar-b.html#c12562" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Basalt</a> bis zu typischen <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimenten</a> (z. B. <a href="glossar-r.html#c12468" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Radiolarit</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12678" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Orogenkeil:</h3><p>Keilförmig angeschoppte <a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Decken</a> eines sich bildenden Gebirges (<a href="glossar-g.html#c12598" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gebirgsbildung</a>). Zumeist werden die jüngsten <a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Decken</a> an der Unterseite des Orogenkeils eingebaut, sodass dieser von der Plattengrenze gegen das nicht verformte Vorland wächst. Durch Komplikationen entwickelt sich aber oft ein komplexer <a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Decken</a>bau.</p></div>
|
||||
|
||||
|
||||
<div id="c12679" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Orthogneis:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> aus einem <a href="glossar-s.html#c12712" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>sauren</a><a href="glossar-m.html#c12656" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>magmatischen</a> Ausgangs<a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gestein</a> (z. B. <a href="glossar-g.html#c12613" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Granit</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12680" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Ozeanboden:</h3><p>In der <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Geologie</a> synonym für <a href="glossar-o.html#c12681" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>ozeanische Kruste</a> verwendet.</p></div>
|
||||
|
||||
|
||||
<div id="c12681" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-275"><h3>Ozeanische Kruste:</h3><p>Jener Teil der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a>, der aus den <a href="glossar-b.html#c12563" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>basischen Gesteinen</a><a href="glossar-g.html#c12408" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gabbro</a> und <a href="glossar-b.html#c12562" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Basalt</a> besteht. Diese dünnere, relativ schwere Kruste baut den <a href="glossar-t.html#c12741" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Tiefsee</a>boden auf und unterlagert damit den Großteil der Ozeane.</p></div>
|
||||
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||||
|
||||
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|
||||
</div>
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|
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<div class="container-fluid toggle-box">
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||||
<div class="toggle-button">» Erdgeschichte</div>
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<div class="toggle-content">
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<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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embed_id: 'timeline-embed', //OPTIONAL USE A DIFFERENT DIV ID FOR EMBED
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<form method="get" id="form_kesearch_pi1" name="form_kesearch_pi1" action="https://www.geosphere.at/rocky-austria/suche/">
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<div id="c13166" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
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<div id="c12994" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
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||||
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||||
</div>
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<div id="maincontent" class="content">
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<div id="c12993" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
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#start-right h3, #sidebar h3, #sidebar h2 {
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font-weight:normal;
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||||
}
|
||||
#maincontent h3 {
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
color: #606c65 !Important;
|
||||
}
|
||||
|
||||
#maincontent-title h1.csc-firstHeader {
|
||||
font-size: 2.2em !important;
|
||||
}
|
||||
#maincontent-title h2 {
|
||||
color: #606c65;
|
||||
margin-top: 0;
|
||||
font-size: 1.6em;
|
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margin-top: 0;
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||||
padding-top: 0;
|
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}
|
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p {
|
||||
margin-top: 0;
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}
|
||||
</style></div>
|
||||
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||||
|
||||
<div id="c12995" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><b>P</b></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c13186" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Paläogeographie:</h3><p>Wissenschaftszweig, zur Rekonstruktion der Erde in früheren Zeiten. Grundlage ist die Auswertung von <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen</a> und <a href="glossar-f.html#c12595" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Fossilien</a>, die z. B. Aufschluss über die Verteilung von Land und Meer geben.</p></div>
|
||||
|
||||
|
||||
<div id="c12866" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Paläoklimatologie:</h3><p>Die Paläoklimatologie versucht die klimatischen Verhältnisse der erdgeschichtlichen Vergangenheit zu rekonstruieren. Daraus können auch Aussagen über das zukünftige Klima der Erde abgeleitet werden. </p></div>
|
||||
|
||||
|
||||
<div id="c12456" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Paläontologie:</h3><p>Wissenschaft von den fossilen (<a href="glossar-f.html#c12595" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Fossil</a>) Lebewesen.</p></div>
|
||||
|
||||
|
||||
<div id="c12682" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Paläotethys:</h3><p>Ehemaliger paläozoischer bis mesozoischer Ozean, der sich am Nordrand von Gondwana öffnete und dessen westlicher Teil bei der Variszischen Gebirgsbildung geschlossen wurde. </p></div>
|
||||
|
||||
|
||||
<div id="c12683" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Pangäa:</h3><p>Vom Perm bis in die Trias existierender Großkontinent, in dem nahezu alle alten Kerne der heutigen Kontinente vereinigt waren.</p></div>
|
||||
|
||||
|
||||
<div id="c12684" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Paragneis:</h3><p>Aus <a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>klastischem</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> durch <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphose</a> gebildeter <a href="glossar-g.html#c12609" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gneis</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12685" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Paratethys:</h3><p>Restmeer, das sich im Zuge der <a href="../glossar.html#c12549" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Alpidischen Gebirgsbildung</a> um die Gebirgszüge und zwischen ihnen bildete. Es bedeckte überwiegend <a href="glossar-k.html#c12641" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kontinentale Kruste</a> und erstreckte sich im Paläogen und Neogen von Frankreich bis nach Zentralasien; das Schwarze und das Kaspische Meer sind heutige Reste der Paratethys.</p></div>
|
||||
|
||||
|
||||
<div id="c12686" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Pegmatit:</h3><p>Außergewöhnlich grobkörniges <a href="glossar-p.html#c12697" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>plutonisches Gestein</a> mit meist granitischer Zusammensetzung, das in Form von Gängen (<a href="glossar-g.html#c12597" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ganggestein</a>) oder Linsen vorkommt; oft reich an <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineralen</a> mit seltenen Elementen und daher häufig Lagerstätten bildend.</p></div>
|
||||
|
||||
|
||||
<div id="c12687" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Penninikum:</h3><p><a href="glossar-t.html#c12738" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Tektonische</a> Einheit in den Alpen, benannt nach den Penninischen Alpen (= Walliser Alpen) der Schweiz.</p></div>
|
||||
|
||||
|
||||
<div id="c12688" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Penninischer Ozean:</h3><p>Östlicher Seitenast des Atlantiks, der sich vom Jura bis zur frühen Kreide öffnete und mit der <a href="../glossar.html#c12549" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Alpidischen Gebirgsbildung</a> wieder geschlossen wurde.</p></div>
|
||||
|
||||
|
||||
<div id="c12689" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Peri-Gondwana:</h3><p>Nördliche Ausläufer von <a href="glossar-g.html#c12610" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gondwana</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12690" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Permafrost:</h3><p>Untergrund, der für mindestens zwei Jahre eine Temperatur von 0 °C nicht überschreitet (Dauerfrostboden).</p></div>
|
||||
|
||||
|
||||
<div id="c12691" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Phyllit:</h3><p>Feinkörniges <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> mit durchgehender Schieferung (<a href="glossar-s.html#c12717" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a>) und seidig glänzenden Bruchflächen, entstanden aus <a href="glossar-t.html#c12743" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>tonig</a>-<a href="glossar-s.html#c12474" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>sandigem</a> Ausgangsmaterial.</p></div>
|
||||
|
||||
|
||||
<div id="c12692" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Pillowlava:</h3><p>Unter Wasser erstarrte polsterförmige Form von <a href="glossar-l.html#c12649" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lava</a>, die durch extrem schnelle Abkühlung beim Austritt entstanden ist; häufig gebildet am <a href="glossar-m.html#c12668" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mittelozeanischen Rücken</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12693" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Plagioklas-Gruppe:</h3><p><a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Silikatische</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a> der <a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Feldspat-Gruppe</a>, die neben Aluminium Kalzium und Natrium in wechselnder Menge enthalten.</p></div>
|
||||
|
||||
|
||||
<div id="c12694" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Plankton:</h3><p>Im Wasser lebende Organismen, deren Bewegungsrichtung hauptsächlich durch Wasserströmungen bestimmt wird.</p></div>
|
||||
|
||||
|
||||
<div id="c12695" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Plattentektonik:</h3><p>Prozesse, welche auf die Bewegung der Lithosphärenplatten (<a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphäre</a>) und ihre Wechselwirkung mit dem <a href="glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdmantel</a> bezogen sind.</p></div>
|
||||
|
||||
|
||||
<div id="c12696" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Pluton:</h3><p>Tiefen<a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteins</a>körper unterschiedlicher Größe und Form.</p></div>
|
||||
|
||||
|
||||
<div id="c12697" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Plutonit:</h3><p><a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatit</a> (Tiefen<a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gestein</a>), welches in der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> durch langsame Abkühlung eines <a href="glossar-m.html#c12438" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmas</a> entsteht. <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristalle</a> sind mit freiem Auge sichtbar.</p></div>
|
||||
|
||||
|
||||
<div id="c12698" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Porphyroid:</h3><p>Schwach <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, entstanden aus paläozoischem <a href="glossar-s.html#c12712" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>saurem</a> oder <a href="glossar-i.html#c12420" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>intermediärem</a><a href="glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Vulkanit</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12699" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Prallhang:</h3><p>Kurvenäußeres Ufer eines Flusses, das durch die dort stärkere Strömung mehr abgetragen wird als das kurveninnere Ufer (Gleithang), wo Material wegen der geringeren Strömung bevorzugt abgelagert wird.</p></div>
|
||||
|
||||
|
||||
<div id="c12700" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Prasinit:</h3><p>Schwach <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorphes</a> gelblichgrünes <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> mit vorwiegend <a href="glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plagioklas</a>, <a href="../glossar.html#c12552" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Amphibol</a> und <a href="glossar-e.html#c12582" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Epidot</a> und mitunter <a href="glossar-c.html#c12571" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Chlorit</a>, entstanden aus <a href="glossar-b.html#c12563" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>basischem</a><a href="glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Vulkanit</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c13227" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Prospektion:</h3><p>Aufsuchung und Erkundung wirtschaftlich nutzbarer Vorkommen <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>mineralischer</a> Rohstoffe.</p></div>
|
||||
|
||||
|
||||
<div id="c12701" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Pyroklastische Ablagerungen:</h3><p>Aus einer heißen „Lawine“ aus Gas, <a href="glossar-l.html#c12649" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lava</a>fragmenten und <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>bruchstücken im Zuge vulkanischer Tätigkeit (<a href="glossar-v.html#c12753" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Vulkanismus</a>) verestigt.</p></div>
|
||||
|
||||
|
||||
<div id="c12702" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-10"><h3>Pyroxen-Gruppe:</h3><p>Grün bis schwarz gefärbte, gedrungene <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikatische</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a>, die neben Eisen und Magnesium auch Kalzium, Aluminium und Natrium in wechselnder Menge enthalten können. Wichtige <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteins</a>bildende <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>gruppe in der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> und im oberen <a href="glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdmantel</a>.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
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|
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|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
||||
<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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<div id="timeline-embed"></div>
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<ul><li class="first col-md-2 col-sm-12"><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="first col-md-2 col-sm-12"><a href="../../service.html">Service</a><ul><li><a href="../download.html">Download</a></li><li><a href="../glossar.html">Glossar</a></li></ul></li></ul>
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embed_id: 'timeline-embed', //OPTIONAL USE A DIFFERENT DIV ID FOR EMBED
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<div id="c13167" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
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<div id="c13174" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
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|
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|
||||
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|
||||
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|
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color: #606c65 !Important;
|
||||
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|
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|
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#maincontent-title h1.csc-firstHeader {
|
||||
font-size: 2.2em !important;
|
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|
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|
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|
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|
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<div id="c12902" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><b>Q</b></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12462" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Quarz:</h3><p><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a> aus Siliziumdioxid (SiO<sub>2</sub>); häufiges <a href="glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>gesteinsbildendes</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a> der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12703" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-50"><h3>Quarzit:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, welches überwiegend aus <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a> besteht und zumeist aus <a href="glossar-s.html#c12711" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sandstein</a> entstanden ist.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
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<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
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<div class="toggle-content">
|
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<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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|
||||
<div id="c13168" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
|
||||
|
||||
</div>
|
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</div>
|
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<div id="c13175" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
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<div id="maincontent" class="content">
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<div id="c12903" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><b>R</b></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12767" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Radiolarien:</h3><p>Einzellige planktonische Mikroorganismen mit meist kugelförmigem Skelett aus Opal (Siliziumdioxid mit Wasser). Sie können als <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>bildner <a href="glossar-r.html#c12468" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Radiolarit</a> aufbauen.</p></div>
|
||||
|
||||
|
||||
<div id="c12468" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Radiolarit:</h3><p><a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a>reiches <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a>, das vorwiegend aus in großer Meerestiefe abgelagerten Skeletten von Radiolarien (planktonische Mikroorganismen mit kugelförmigem Skelett; <a href="glossar-p.html#c12694" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plankton</a>) entstanden ist.</p></div>
|
||||
|
||||
|
||||
<div id="c12704" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Radiometrische Altersbestimmung:</h3><p>Auf dem radioaktiven Zerfall von Atomen beruhende Methode in der <a href="glossar-g.html#c12600" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Geochronologie</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12705" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Rheischer Ozean:</h3><p>Ehemaliger, frühpaläozoischer Ozean zwischen <a href="glossar-g.html#c12610" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gondwana</a> und <a href="glossar-l.html#c12648" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Laurussia</a>, der im Zuge der <a href="glossar-v.html#c12492" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Variszischen Gebirgsbildung</a> geschlossen wurde.</p></div>
|
||||
|
||||
|
||||
<div id="c13188" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Rhenodanubisch:</h3><p>Diese Bezeichnung leitet sich von den lateinischen Namen für die Flüsse Rhein (Rhenus) und Donau (Danubius) ab und wird oft in Zusammenhang mit der West-Osterstreckung der <a href="glossar-f.html#c12593" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Flysch</a>zone verwendet. </p></div>
|
||||
|
||||
|
||||
<div id="c12706" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Rhyolith:</h3><p><a href="glossar-s.html#c12712" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Saures</a><a href="glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>vulkanisches</a><a href="glossar-s.html#c12712" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, welches aus größeren <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristallen</a> von <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a> und Alkali<a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>feldspat</a>, oft auch <a href="glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plagioklas</a> und <a href="glossar-b.html#c12755" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Biotit</a> in einer glasigen Grundmasse besteht, die eine chemische Zusammensetzung wie <a href="glossar-g.html#c12613" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Granit</a> besitzt.</p></div>
|
||||
|
||||
|
||||
<div id="c12707" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Riff:</h3><p>Erhebung auf dem Boden eines Gewässers. Korallenriffe bestehen aus den Skeletten von Korallen und anderen <a href="glossar-k.html#c12623" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalk</a> abscheidenden Organismen; auch die Schalen von Muscheln können Riffe aufbauen.</p></div>
|
||||
|
||||
|
||||
<div id="c12708" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Riffkalk:</h3><p>Überwiegend von riffbildenden Organismen (Korallen, Kalkalgen, Schwämme etc.) aufgebauter <a href="glossar-k.html#c12623" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kalk(stein)</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12709" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Rift:</h3><p>Grabenbruch in <a href="glossar-k.html#c12641" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kontinentaler Kruste</a> durch Zerreißen und beginnendes Auseinanderdriften von <a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphären</a>platten, von <a href="glossar-v.html#c12753" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Vulkanismus</a> begleitet.</p></div>
|
||||
|
||||
|
||||
<div id="c12710" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-50"><h3>Rutschung:</h3><p>Hangabwärts gerichtete Verlagerungen von <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimenten</a> oder aufgelockerten <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteinen</a> unter der Wirkung der Schwerkraft.</p></div>
|
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||||
|
||||
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<div class="toggle-button">» Erdgeschichte</div>
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<script src="../../../fileadmin/template-rocky/js/jquery-1.11.1.min.js"></script>
|
||||
<script src="../../../fileadmin/template-rocky/js/jquery.fancybox.pack.js"></script>
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<script type="text/javascript" src="../../../fileadmin/template/js/jquery.textresizer.min.js"></script>
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<script src="../../../fileadmin/template-rocky/js/helpers/jquery.fancybox-buttons.js"></script>
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<script src="../../../../unpkg.com/popper.js%401.16.1/dist/umd/popper.min.js"></script>
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<script src="../../../../unpkg.com/tooltip.js%401.3.3/dist/umd/tooltip.min.js"></script>
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||||
|
||||
<!-- <script type="text/javascript" src="https://s3.amazonaws.com/cdn.knightlab.com/libs/timeline/latest/js/storyjs-embed.js"></script>-->
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<script src="../../../fileadmin/template-rocky/timeline/build/js/storyjs-embed.js"></script>
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||||
<script src="../../../fileadmin/template-rocky/js/responsive-map.js"></script>
|
||||
<script src="../../../fileadmin/template-rocky/js/script.js"></script>
|
||||
|
||||
<script>
|
||||
$(document).ready(function() {
|
||||
createStoryJS({
|
||||
type: 'timeline',
|
||||
width: '800',
|
||||
height: '600',
|
||||
source: '/fileadmin/template-rocky/timeline/example_json.json',
|
||||
embed_id: 'timeline-embed', //OPTIONAL USE A DIFFERENT DIV ID FOR EMBED
|
||||
});
|
||||
});
|
||||
</script>
|
||||
<link rel="canonical" href="glossar-s.html">
|
||||
</head>
|
||||
<body id="page-769">
|
||||
<div class="container-fluid background">
|
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<div class="row-fluid">
|
||||
<div class="col-md-5 logo-container">
|
||||
<a href="../../index.html"><img src="../../../fileadmin/template-rocky/img/logo.jpg" alt="Rocky"></a>
|
||||
</div>
|
||||
<div class="col-md-7">
|
||||
<div class="header-maps">
|
||||
<div class="switch">
|
||||
<a href="#" data-target="landschaften">Landschaften</a> | <a href="#" data-target="bausteine">Bausteine</a>
|
||||
</div>
|
||||
<object id="landschaften" class="landschaften map" data="../../fileadmin/template-rocky/img/Karte_Landschaften.svg" type="image/svg+xml">
|
||||
Ihr Browser kann leider kein SVG darstellen.
|
||||
</object>
|
||||
<object id="bausteine" class="bausteine map" data="../../fileadmin/template-rocky/img/Karte_Bausteine.svg" type="image/svg+xml" style="display:none;">
|
||||
Ihr Browser kann leider kein SVG darstellen.
|
||||
</object>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
<div class="row">
|
||||
<div class="col-md-10">
|
||||
<nav id="mainnav">
|
||||
<ul><li><a href="../../landschaften.html">Landschaften</a><ul class="scndLevel clearfix"><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../../grundlagen.html">Grundlagen</a><ul class="scndLevel clearfix"><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../../bausteine.html">Bausteine</a><ul class="scndLevel clearfix"><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul class="scndLevel clearfix"><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="selected"><a href="../../service.html" class="selected">Service</a><ul class="scndLevel clearfix"><li><a href="../download.html">Download</a></li><li class="selected"><a href="../glossar.html" class="selected">Glossar</a></li></ul></li></ul>
|
||||
|
||||
</nav>
|
||||
<div id="mobile-nav">
|
||||
<ul><li><a href="#">Menü</a><ul><li><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li class="last"><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li class="last"><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li class="last"><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li class="last"><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="last"><a href="../../service.html" class="active">Service</a><ul><li><a href="../download.html">Download</a></li><li class="last"><a href="../glossar.html" class="active">Glossar</a></li></ul></li></ul></li></ul>
|
||||
</div>
|
||||
</div>
|
||||
<div class="col-md-2">
|
||||
<div class="container-right-top clearfix">
|
||||
<div id="language">
|
||||
<ul></ul>
|
||||
</div>
|
||||
<div id="textSizer">
|
||||
<div class="fontSize hidden-sm hidden-xs" id="fontsize">
|
||||
<p>
|
||||
<a href="#nogo" class="">
|
||||
<span class="medium">A</span>
|
||||
</a>
|
||||
<a href="#nogo" class="">
|
||||
<span class="large">A</span>
|
||||
</a>
|
||||
</p>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
<div class="container-right-bottom">
|
||||
<div class="search-container">
|
||||
<!--<form action="index.php?id=803" method="post" id="indexedsearch">
|
||||
<input type="hidden" name="tx_indexedsearch[sections]" value="0">
|
||||
<input name="tx_indexedsearch[submit_button]" value="Search" type="hidden">
|
||||
<input name="tx_indexedsearch[sword]" placeholder="Suchbegriff" id="search-field" type="text">
|
||||
<input type="image" src="/fileadmin/template-rocky/img/search.png" id="search-button" class="searchButton" alt="Search" title="Search">
|
||||
</form>-->
|
||||
<form method="get" id="form_kesearch_pi1" name="form_kesearch_pi1" action="https://www.geosphere.at/rocky-austria/suche/">
|
||||
<fieldset class="kesearch_searchbox">
|
||||
<!-- <input type="hidden" name="id" value="803"> -->
|
||||
<!-- <input type="text" id="ke_search_sword" name="tx_kesearch_pi1[sword]" value="" placeholder="Suchbegriff" onfocus="if (this.value == 'Suchbegriff') { this.value = ''; }" onblur="if (this.value == '') { this.value = 'Suchbegriff'; }">
|
||||
<input type="image" src="../../../fileadmin/template-rocky/img/search.png" id="search-button" class="searchButton" alt="Search" title="Suche"> -->
|
||||
<input id="kesearchpagenumber" type="hidden" name="tx_kesearch_pi1[page]" value="1">
|
||||
<input id="resetFilters" type="hidden" name="tx_kesearch_pi1[resetFilters]" value="0">
|
||||
<input id="sortByField" type="hidden" name="tx_kesearch_pi1[sortByField]" value="">
|
||||
<input id="sortByDir" type="hidden" name="tx_kesearch_pi1[sortByDir]" value="">
|
||||
</fieldset>
|
||||
</form>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
|
||||
<div class="row custom-row" id="pageWrap">
|
||||
|
||||
<div class="col-md-3 custom-column">
|
||||
<div id="sidebar" class="content">
|
||||
|
||||
<div id="c13169" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
<div class="col-md-9 custom-column">
|
||||
<div id="maincontent-title" class="content">
|
||||
|
||||
<div id="c13176" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
|
||||
|
||||
<div id="c13152" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
|
||||
#start-right h3, #sidebar h3, #sidebar h2 {
|
||||
margin-top: 0;
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
|
||||
}
|
||||
#maincontent h3 {
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
color: #606c65 !Important;
|
||||
}
|
||||
|
||||
#maincontent-title h1.csc-firstHeader {
|
||||
font-size: 2.2em !important;
|
||||
}
|
||||
#maincontent-title h2 {
|
||||
color: #606c65;
|
||||
margin-top: 0;
|
||||
font-size: 1.6em;
|
||||
margin-top: 0;
|
||||
padding-top: 0;
|
||||
}
|
||||
p {
|
||||
margin-top: 0;
|
||||
}
|
||||
</style></div>
|
||||
|
||||
|
||||
<div id="c12904" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><b>S</b></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12474" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Sand:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klastisches</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> im Korngrößenbereich von 0,063 mm bis 2 mm.</p></div>
|
||||
|
||||
|
||||
<div id="c12711" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Sandstein:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klastisches</a><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a> im Korngrößenbereich von 0,063 mm bis 2 mm.</p></div>
|
||||
|
||||
|
||||
<div id="c12712" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Saures Gestein:</h3><p><a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatisches Gestein</a> mit einem hohen SiO<sub>2</sub>-Gehalt von mehr als 63 %.</p></div>
|
||||
|
||||
|
||||
<div id="c12713" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schelf:</h3><p>Randbereich der Kontinente, der bis ca. 200 m Wassertiefe unter dem Meeresspiegel liegt.</p></div>
|
||||
|
||||
|
||||
<div id="c12714" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schelfmeer:</h3><p>Flachwasserbereich am <a href="glossar-s.html#c12713" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schelf</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12715" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schichtflut:</h3><p>Flächenhafter, schlammbeladener Wasserabfluss auf leicht geneigter Ebene.</p></div>
|
||||
|
||||
|
||||
<div id="c12716" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schichtlücke:</h3><p><a href="glossar-s.html#c13190" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Stratigraphische</a> Lücke innerhalb einer durchgehenden Ablagerung von <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a>, hervorgerufen durch Unterbrechung der <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a>ation und eventuell zusätzlich <a href="glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erosion</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c13189" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schichtfolge:</h3><p>Bezeichnung für kontinuierlich übereinander abgelagerte <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>sschichten, die eine Entwicklungsgeschichte erzählen, z. B. von Seicht- zu Tiefwasserablagerungen.</p></div>
|
||||
|
||||
|
||||
<div id="c12717" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schiefer:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> mit einer schiefrigen Struktur und einer Spaltbarkeit von unter 1 cm. Der Gehalt an <a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Feldspat</a> liegt unter 20 % und ein Lagenbau ist gewöhnlich vorhanden.</p></div>
|
||||
|
||||
|
||||
<div id="c12718" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schieferton:</h3><p>Geschichtetes <a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>klastisches</a><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a> mit einer Korngröße < 0.002 mm.</p></div>
|
||||
|
||||
|
||||
<div id="c12719" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schlier:</h3><p>Informelle Bezeichnung für fein<a href="glossar-s.html#c12474" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>sandig</a>-schluffigen (<a href="glossar-s.html#c12720" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schluff</a>) Mergel im Bereich der <a href="glossar-m.html#c12670" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Molasse</a>zone und des Steirischen Beckens.</p></div>
|
||||
|
||||
|
||||
<div id="c12720" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schluff:</h3><p>Alternativer Name für <a href="glossar-s.html#c12731" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Silt</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12721" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schotter:</h3><p>Besteht hauptsächlich aus <a href="glossar-k.html#c12631" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kies</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12722" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schuppe:</h3><p>Subeinheit einer <a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Decke</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12723" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Sediment:</h3><p>Entsteht durch Ablagerung von <a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>klastischem</a> Material, das durch Luft, Wasser, Eis, Wind transportiert wird, oder aus Material, welches sich durch chemische Fällung aus Lösung bzw. aus Abscheidung durch Organismen bildet. Formt lockere, nicht konsolidierte Lagen und Körper an der Erdoberfläche.</p></div>
|
||||
|
||||
|
||||
<div id="c12724" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Sedimentgestein:</h3><p>Verfestigtes <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a>, welches durch Entwässerung, Volumenverkleinerung, Zementbildung oder biogene Verkittung entsteht (<a href="glossar-d.html#c12572" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Diagenese</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12725" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Seife:</h3><p>Örtliche Anhäufung von spezifisch schweren <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineralen</a> in <a href="glossar-s.html#c12474" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sand </a>oder <a href="glossar-k.html#c12631" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kies</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12726" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Seitenverschiebung:</h3><p>Eine steil stehende bis vertikale <a href="glossar-s.html#c12734" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Störung</a> mit überwiegend horizontaler Verschiebung der angrenzenden <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>körper.</p></div>
|
||||
|
||||
|
||||
<div id="c12727" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Serpentin-Gruppe:</h3><p>Feinblättrige, sehr magnesiumreiche Schicht<a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikate</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12728" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Serpentinit:</h3><p>Grünes bis schwarzes <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a>, welches vornehmlich aus <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineralen</a> der <a href="glossar-s.html#c12727" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Serpentin-Gruppe</a> besteht, gebildet durch Wasseraufnahme von <a href="glossar-u.html#c12750" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ultrabasit</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12730" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Sibiria:</h3><p>Ehemaliger proterozoischer bis paläozoischer Kontinent, der im Perm im Zuge der <a href="glossar-g.html#c12598" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gebirgsbildung</a> des Ural dem Großkontinent <a href="glossar-p.html#c12683" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pangäa</a> angegliedert wurde.</p></div>
|
||||
|
||||
|
||||
<div id="c12729" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Silikate:</h3><p>Salze verschiedener <a href="glossar-k.html#c12634" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kieselsäuren</a>; einfache Silikat-Ionen bestehen aus SiO<sub>4</sub>-Tetraedern, die zu verschiedenen Strukturen wie beispielsweise Ketten-, Schicht- oder Gerüstsilikaten verknüpft sind. Natürliche Silikate spielen eine große Rolle in der <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Geologie</a>, da sehr viele <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a> dieser Stoffgruppe angehören. Die <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> besteht zu über 90 Prozent, der <a href="glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdmantel</a> fast vollständig aus Silikaten.</p></div>
|
||||
|
||||
|
||||
<div id="c12731" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Silt:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klastisches</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> im Korngrößenbereich zwischen 0,002 und 0,063 mm, auch als <a href="glossar-s.html#c12720" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schluff</a> bezeichnet.</p></div>
|
||||
|
||||
|
||||
<div id="c12732" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Siltstein:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klastisches</a><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a> im Korngrößenbereich zwischen 0,002 und 0,063 mm.</p></div>
|
||||
|
||||
|
||||
<div id="c13226" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Spurenfossilien:</h3><p>Hinweise in <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimenten</a> auf Vorkommen, Lebensumstände und Verhalten <a href="glossar-f.html#c12595" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>fossiler</a> Organismen zu Lebzeiten.</p></div>
|
||||
|
||||
|
||||
<div id="c12733" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Steinsalz:</h3><p>Chemisches <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a>, das zu mehr als der Hälfte aus grob <a href="glossar-k.html#c12645" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>kristallinem</a> Salz (Natriumchlorid) besteht, typischerweise durch Eisenoxide gefärbt und mit <a href="glossar-t.html#c12743" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ton</a> vermischt.</p></div>
|
||||
|
||||
|
||||
<div id="c13190" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Stratigraphie:</h3><p>Teilgebiet der Historischen Geologie, das die zeitliche und räumliche Ordnung der Gesteine unter Berücksichtigung aller physikalischen und chemischen Grundmerkmale (Fossilinhalt, Zusammensetzung etc.) zum Ziel hat. Sie ist somit Basis und Maßstab für die Klärung und Parallelisierung erdgeschichtlicher und regionalgeologischer Prozesse.</p></div>
|
||||
|
||||
|
||||
<div id="c12734" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Störung:</h3><p>Grenzfläche, die zwei <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>einheiten trennt und an der Bewegung stattgefunden hat.</p></div>
|
||||
|
||||
|
||||
<div id="c13225" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Strömungsmarken:</h3><p><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentäre</a><a href="glossar-s.html#c12735" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Strukturen</a>, die als <a href="glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erosions</a>formen auf <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a>oberflächen durch darüber strömendes Wasser entstehen.</p></div>
|
||||
|
||||
|
||||
<div id="c12735" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Struktur:</h3><p>In der <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Geologie</a> die generelle Anordnung von <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>massen, insbesondere Lage, Gefüge (<a href="glossar-g.html#c12599" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gefügekunde</a>) oder relative Position in einem Gebiet oder einer Region.</p></div>
|
||||
|
||||
|
||||
<div id="c12736" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Subduktion:</h3><p>Abtauchen einer Lithosphärenplatte (<a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphäre</a>) unter eine andere.</p></div>
|
||||
|
||||
|
||||
<div id="c13223" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-5"><h3>Subpenninikum:</h3><p>Bezeichnung für die <a href="glossar-t.html#c12738" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>tektonische</a> Lage dieser Einheit unter den <a href="glossar-p.html#c12687" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Penninischen</a><a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Decken</a>, also in „sub“penninischer Position.</p></div>
|
||||
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||||
|
||||
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|
||||
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||||
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<div class="container-fluid toggle-box">
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<div class="toggle-button">» Erdgeschichte</div>
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<div class="toggle-content">
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<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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<a href="#nogo" class="">
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<span class="medium">A</span>
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||||
<a href="#nogo" class="">
|
||||
<span class="large">A</span>
|
||||
</a>
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</form>-->
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<form method="get" id="form_kesearch_pi1" name="form_kesearch_pi1" action="https://www.geosphere.at/rocky-austria/suche/">
|
||||
<fieldset class="kesearch_searchbox">
|
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<!-- <input type="text" id="ke_search_sword" name="tx_kesearch_pi1[sword]" value="" placeholder="Suchbegriff" onfocus="if (this.value == 'Suchbegriff') { this.value = ''; }" onblur="if (this.value == '') { this.value = 'Suchbegriff'; }">
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<input id="sortByField" type="hidden" name="tx_kesearch_pi1[sortByField]" value="">
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<input id="sortByDir" type="hidden" name="tx_kesearch_pi1[sortByDir]" value="">
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</fieldset>
|
||||
</form>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
</div>
|
||||
|
||||
<div class="row custom-row" id="pageWrap">
|
||||
|
||||
<div class="col-md-3 custom-column">
|
||||
<div id="sidebar" class="content">
|
||||
|
||||
<div id="c13170" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
<div class="col-md-9 custom-column">
|
||||
<div id="maincontent-title" class="content">
|
||||
|
||||
<div id="c13177" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
|
||||
|
||||
<div id="c13181" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
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||||
#start-right h3, #sidebar h3, #sidebar h2 {
|
||||
margin-top: 0;
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
|
||||
}
|
||||
#maincontent h3 {
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
||||
color: #606c65 !Important;
|
||||
}
|
||||
|
||||
#maincontent-title h1.csc-firstHeader {
|
||||
font-size: 2.2em !important;
|
||||
}
|
||||
#maincontent-title h2 {
|
||||
color: #606c65;
|
||||
margin-top: 0;
|
||||
font-size: 1.6em;
|
||||
margin-top: 0;
|
||||
padding-top: 0;
|
||||
}
|
||||
p {
|
||||
margin-top: 0;
|
||||
}
|
||||
</style></div>
|
||||
|
||||
|
||||
<div id="c12905" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><b>T</b></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12480" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Talgletscher:</h3><p>Gletscherstrom in Talbereichen.</p></div>
|
||||
|
||||
|
||||
<div id="c12737" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Tektonik:</h3><p>Lehre vom Aufbau der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> sowie den Bewegungen und Kräften, welche die <a href="glossar-s.html#c12735" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Strukturen</a> erzeugt haben.</p></div>
|
||||
|
||||
|
||||
<div id="c12738" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Tektonisch:</h3><p>Auf die Bewegungen und Kräfte in der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> bezogen.</p></div>
|
||||
|
||||
|
||||
<div id="c12739" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Terrasse:</h3><p>Abstufung im Gelände, insbesondere Felsoder <a href="glossar-s.html#c12721" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schotter</a>stufe an Talhängen. Terrassen lassen auf die Lage eines ursprünglichen Flussbettes (<a href="glossar-f.html#c12592" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Flussterrasse</a>), eines Seeufers oder eines Meeresstrandes schließen.</p></div>
|
||||
|
||||
|
||||
<div id="c12740" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Tethys:</h3><p>Ozean, der sich im Perm am Südostrand von <a href="glossar-p.html#c12683" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Pangäa</a> öffnete und im Zuge der <a href="../glossar.html#c12549" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Alpidischen Gebirgsbildung</a> weitgehend geschlossen wurde. Das östliche Mittelmeer ist ein Rest der Tethys. Der Name leitet sich von Tethys, einer Titanin der griechischen Mythologie, der Schwester und Gemahlin des Okeanos ab.</p></div>
|
||||
|
||||
|
||||
<div id="c12741" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Tiefsee:</h3><p>In der <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Geologie</a> der Ablagerungsbereich unterhalb von 4 000 m und in der Meeresbiologie der lichtlose Bereich des Meeres in mehr als 800 m Tiefe.</p></div>
|
||||
|
||||
|
||||
<div id="c12742" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Tiefseerinne:</h3><p>Asymmetrische Rinne im <a href="glossar-t.html#c12741" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Tiefsee</a>boden mit Tiefen bis über 11 000 m; topographischer Ausdruck der <a href="glossar-s.html#c12736" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Subduktion</a> einer <a href="glossar-o.html#c12681" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>ozeanischen</a><a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Lithosphären</a>platte.</p></div>
|
||||
|
||||
|
||||
<div id="c12743" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Ton:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Klastisches</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sediment</a> mit einer Korngröße < 0,002 mm.</p></div>
|
||||
|
||||
|
||||
<div id="c12744" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Tonalit:</h3><p><a href="glossar-p.html#c12697" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plutonisches Gestein</a>, welches aus <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Quarz</a>, <a href="glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plagioklas</a> sowie <a href="../glossar.html#c12552" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Amphibol</a> und <a href="glossar-b.html#c12755" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Biotit</a> besteht.</p></div>
|
||||
|
||||
|
||||
<div id="c12745" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Tonschiefer:</h3><p>Äußerst feinkörniges, schwach <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> mit durchgehender schiefriger Spaltbarkeit (<a href="glossar-s.html#c12717" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Schiefer</a>); entsteht aus <a href="glossar-t.html#c12746" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Tonstein</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c12746" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Tonstein:</h3><p>Ungeschichtetes <a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>klastisches</a><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimentgestein</a> mit einer Korngröße < 0,002 mm.</p></div>
|
||||
|
||||
|
||||
<div id="c13233" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Trogtäler:</h3><p>U-förmige Trogtäler stellen eine spezifisch <a href="glossar-g.html#c12606" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>glaziale</a><a href="glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erosions</a>form dar, während die einschneidende Wirkung des Wassers Täler mit V-förmigem Querschnitt erzeugt.</p></div>
|
||||
|
||||
|
||||
<div id="c12747" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Trübestrom:</h3><p>Schnell fließende Wassermassen mit reichlich <a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>klastischem</a> Material; häufig an unterseeischen Hängen, meist durch Erdbeben ausgelöst.</p></div>
|
||||
|
||||
|
||||
<div id="c12748" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Tuff:</h3><p><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gestein</a> aus verfestigten, feinkörnigen vulkanischen Auswurfprodukten (<a href="glossar-v.html#c12753" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Vulkanismus</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12749" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-85"><h3>Turbidit:</h3><p>Verfestigte Ablagerungen eines <a href="glossar-t.html#c12747" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Trübestroms</a>.</p></div>
|
||||
|
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|
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</div>
|
||||
</div>
|
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|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
||||
<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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<div id="timeline-embed"></div>
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<ul><li class="first col-md-2 col-sm-12"><a href="../../landschaften.html">Landschaften</a><ul><li><a href="../../landschaften/boehmische-masse.html">Böhmische Masse</a></li><li><a href="../../landschaften/alpenvorland.html">Alpenvorland</a></li><li><a href="../../landschaften/voralpen.html">Voralpen</a></li><li><a href="../../landschaften/noerdliche-kalkalpen.html">Nördliche Kalkalpen</a></li><li><a href="../../landschaften/zentrale-ostalpen.html">Zentrale Ostalpen</a></li><li><a href="../../landschaften/suedalpen.html">Südalpen</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../grundlagen.html">Grundlagen</a><ul><li><a href="../../grundlagen/plattentektonik.html">Plattentektonik</a></li><li><a href="../../grundlagen/gesteinskreislauf.html">Gesteinskreislauf</a></li><li><a href="../../grundlagen/fossilien.html">Fossilien</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../bausteine.html">Bausteine</a><ul><li><a href="../../bausteine/moldanubikum-moravikum.html">Moldanubikum-Moravikum</a></li><li><a href="../../bausteine/helvetikum.html">Helvetikum</a></li><li><a href="../../bausteine/subpennin.html">Subpennin</a></li><li><a href="../../bausteine/pennin.html">Pennin</a></li><li><a href="../../bausteine/ostalpin.html">Ostalpin</a></li><li><a href="../../bausteine/sudalpin.html">Südalpin</a></li><li><a href="../../bausteine/meliatikum.html">Meliatikum</a></li><li><a href="../../bausteine/molasse.html">Molasse</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../entwicklungsgeschichte.html">Entwicklungsgeschichte</a><ul><li><a href="../../entwicklungsgeschichte/pra-kambrium.html">(Prä-)Kambrium</a></li><li><a href="../../entwicklungsgeschichte/ordoviz-silur-devon.html">Ordoviz, Silur, Devon</a></li><li><a href="../../entwicklungsgeschichte/karbon.html">Karbon</a></li><li><a href="../../entwicklungsgeschichte/perm.html">Perm</a></li><li><a href="../../entwicklungsgeschichte/trias.html">Trias</a></li><li><a href="../../entwicklungsgeschichte/jura.html">Jura</a></li><li><a href="../../entwicklungsgeschichte/kreide.html">Kreide</a></li><li><a href="../../entwicklungsgeschichte/palaogen.html">Paläogen</a></li><li><a href="../../entwicklungsgeschichte/neogen.html">Neogen</a></li><li><a href="../../entwicklungsgeschichte/quartar.html">Quartär</a></li></ul></li><li class="first col-md-2 col-sm-12"><a href="../../gebirgsbildung.html">Gebirgsbildung</a></li><li class="first col-md-2 col-sm-12"><a href="../../service.html">Service</a><ul><li><a href="../download.html">Download</a></li><li><a href="../glossar.html">Glossar</a></li></ul></li></ul>
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<div id="c13171" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
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Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
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</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
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<div id="c13178" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
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Glossar
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</span></h1><h2 class="">
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Begriffe von A - Z
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<div id="c12906" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><b>U</b></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">» </span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12486" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Überschiebung:</h3><p>Geneigte <a href="glossar-s.html#c12734" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Störung</a>, an der ein <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>paket nach oben versetzt wurde. Entsteht durch Einengung der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> bei der <a href="glossar-g.html#c12598" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gebirgsbildung</a> (<a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Decke</a>).</p></div>
|
||||
|
||||
|
||||
<div id="c12750" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Ultrabasit:</h3><p><a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatisches Gestein</a> mit einem sehr geringen SiO<sub>2</sub>-Gehalt von weniger als 45 %, das den oberen <a href="glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdmante</a>l aufbaut.</p></div>
|
||||
|
||||
|
||||
<div id="c12751" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Unterostalpin:</h3><p>Subeinheit des Ostalpins, die ehemals am Nordrand des „<a href="../glossar.html#c12546" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Adria</a>tischen Sporns“ bzw. der Adriatischen Platte hin zum <a href="glossar-p.html#c12688" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Penninischen Ozean</a> gelegen ist und nun die <a href="glossar-t.html#c12738" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>tektonisch</a> tiefsten Anteile des Ostalpins bildet.</p></div>
|
||||
|
||||
|
||||
<div id="c13185" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-205"><h3>Unterströmungstheorie:</h3><p>Dieses Konzept beruht auf der Annahme von <a href="glossar-k.html#c12643" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Konvektionsströmungen </a>in zähplastischen Tiefenzonen der Erde, welche die Bewegung der Kontinente verursachen. Im Unterschied zur modernen Theorie der <a href="glossar-p.html#c12695" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Plattentektonik </a>steigen nach diesem Konzept die heißen Massen aber unter den Kontinenten auf, fließen von dort unter die „Kühlfläche“ der <a href="glossar-o.html#c12680" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Ozeanböden </a>und sinken schließlich wieder in die Tiefe.</p></div>
|
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|
||||
|
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</div>
|
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</div>
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</div>
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<div class="container-fluid toggle-box">
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<div class="toggle-button">» Erdgeschichte</div>
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<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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|
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||||
<div id="c13172" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
|
||||
Detail aus dem Glasmosaik „Reichtum Erde“ von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. © Geologische Bundesanstalt
|
||||
</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
|
||||
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
|
||||
|
||||
|
||||
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|
||||
</div>
|
||||
<div class="col-md-9 custom-column">
|
||||
<div id="maincontent-title" class="content">
|
||||
|
||||
<div id="c13179" class="frame frame-default frame-type-header frame-layout-0 frame-space-before-standard frame-space-after-standard"><h1 class="element-header "><span>
|
||||
Glossar
|
||||
</span></h1><h2 class="">
|
||||
Begriffe von A - Z
|
||||
</h2></div>
|
||||
|
||||
|
||||
</div>
|
||||
<div id="maincontent" class="content">
|
||||
|
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<div id="c13183" class="frame frame-default frame-type-html frame-layout-0 frame-space-before-standard frame-space-after-standard"><style type="text/css">
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#start-right h3, #sidebar h3, #sidebar h2 {
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margin-top: 0;
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font-size: 1.2em;
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font-weight:normal;
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}
|
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#maincontent h3 {
|
||||
font-size: 1.2em;
|
||||
font-weight:normal;
|
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color: #606c65 !Important;
|
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|
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|
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#maincontent-title h1.csc-firstHeader {
|
||||
font-size: 2.2em !important;
|
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|
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#maincontent-title h2 {
|
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|
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margin-top: 0;
|
||||
font-size: 1.6em;
|
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margin-top: 0;
|
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padding-top: 0;
|
||||
}
|
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p {
|
||||
margin-top: 0;
|
||||
}
|
||||
</style></div>
|
||||
|
||||
|
||||
<div id="c12907" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">» </span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">» </span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">» </span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">» </span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">» </span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">» </span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">» </span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">» </span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">» </span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">» </span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">» </span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">» </span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">» </span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">» </span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">» </span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">» </span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">» </span><b>R</b></a></td><td rowspan="1"><a href="glossar-s.html" title="Im selben Fenster: Glossar Buchstabe S" class="internal-link"><span class="link-prefix">» </span><b>S</b></a></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">» </span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">» </span><b>U</b></a></td><td rowspan="1"><b>V</b></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">» </span><b>Z</b></a></td></tr></tbody></table></div>
|
||||
|
||||
|
||||
<div id="c12492" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Variszische Gebirgsbildung:</h3><p>Entstehung der spätpaläozoischen Gebirge, deren Reste große Gebiete Mittel- und Westeuropas prägen; auch in den Alpen sind überformte Teile eines variszischen Gebirges nachweisbar.</p></div>
|
||||
|
||||
|
||||
<div id="c12752" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Verwitterung:</h3><p>Beinhaltet alle physikalischen und chemischen Prozesse die an oder nahe der Erdoberfläche <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Sedimente</a> oder <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteine</a> zersetzt beziehungsweise auflockert. Die Verwitterung ist ein Vorgang der <a href="glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erosion</a>.</p></div>
|
||||
|
||||
|
||||
<div id="c13232" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Vorlandbecken:</h3><p>Ein Becken, das durch die Auflast eines herannahenden <a href="glossar-o.html#c12678" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Orogenkeils</a> entsteht.</p></div>
|
||||
|
||||
|
||||
<div id="c12753" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Vulkanismus:</h3><p>Zusammenfassender Begriff für alle Prozesse, die mit Aufstieg von <a href="glossar-m.html#c12438" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magma</a> an die Erdoberfläche verbunden sind.</p></div>
|
||||
|
||||
|
||||
<div id="c12754" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-5"><h3>Vulkanit:</h3><p><a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Magmatit</a>, gebildet in Verbindung mit <a href="glossar-v.html#c12753" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Vulkanismus</a>; durch rasche Abkühlung meist sehr feinkörnig; mit freiem Auge sichtbar sind nur einzelne gröbere <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Kristalle</a>, sogenannte „Einsprenglinge“.</p></div>
|
||||
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
</div>
|
||||
</div>
|
||||
|
||||
|
||||
<div class="container-fluid toggle-box">
|
||||
<div class="toggle-button">» Erdgeschichte</div>
|
||||
<div class="toggle-content">
|
||||
<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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<div id="timeline-embed"></div>
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267
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<div id="c13173" class="frame frame-default frame-type-shortcut frame-layout-0 frame-space-before-standard frame-space-after-standard"><div id="c7374" class="frame frame-default frame-type-textpic frame-layout-0 frame-space-before-standard frame-space-after-standard"><div class="ce-textpic ce-center ce-above"><div class="ce-gallery" data-ce-columns="1" data-ce-images="1"><div class="ce-outer"><div class="ce-inner"><div class="ce-row"><div class="ce-column"><figure class="image"><img class="image-embed-item" title="Glasmosaik" alt="Kunstwerk" src="../../../fileadmin/_processed_/3/3/csm_mosaik_427ff9a400.jpg" width="600" height="452" loading="lazy"><figcaption class="image-caption">
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</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren Füßen, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, zählen seit jeher zu den natürlichen Grundfragen des Menschen.
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</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist häufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bedürfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verständlich erläutert werden!</p></div></div></div></div>
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<div id="c12498" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Zirkon:</h3><p>Sehr stabiles <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>silikatisches</a> Zirkonium-<a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Mineral</a>, das in vielen <a href="glossar-s.html#c12712" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>sauren Gesteinen</a> in geringen Mengen vorkommt. Die ältesten <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Minerale</a> der <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Erdkruste</a> sind Zirkone, da diese den <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">» </span>Gesteins</a>kreislauf mehrfach durchlaufen können.</p></div>
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