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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">
Detail aus dem Glasmosaik &bdquo;Reichtum Erde&ldquo; von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. &copy; 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 F&uuml;&szlig;en, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, z&auml;hlen seit jeher zu den nat&uuml;rlichen 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 h&auml;ufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bed&uuml;rfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verst&auml;ndlich erl&auml;utert werden!</p></div></div></div></div>
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Glossar
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Begriffe von A - Z
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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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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=
<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">&raquo;&nbsp;</span>St&ouml;rung</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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 St&uuml;ck kontinentaler <a href="glossar/glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Lithosph&auml;re</a>, das seit der fr&uuml;hen Oberkreide einen Teil der Adriatischen Platte bildet. Davor war dieses St&uuml;ck ein Fortsatz am Nordrand des heutigen afrikanischen Kontinents, der auch als &bdquo;Adriatischer Sporn&ldquo; bezeichnet wird. Seit der &Ouml;ffnung des <a href="glossar/glossar-p.html#c12688" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Penninischen Ozeans</a> wurde der &bdquo;Adriatische Sporn&ldquo; bzw. die <a href="glossar/glossar-k.html#c12641" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>kontinentale Kruste</a> der Adriatischen Platte zeitweise vom Meer &uuml;berflutet 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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Akkretion</a>) von Gesteinen, die in einer Subduktionszone von einer ozeanischen Lithosph&auml;renplatte 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 Transportvorg&auml;nge in fremde Umgebung verbracht. Im kleineren Ma&szlig;stab k&ouml;nnen dies <a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gesteins</a>bruchst&uuml;cke, Ger&ouml;lle und Gletschergeschiebe (<a href="glossar/glossar-e.html#c12586" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Geschiebe</a>) sein, im gr&ouml;&szlig;eren Ma&szlig;stab Rutschmassen (<a href="glossar/glossar-r.html#c12710" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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 sp&auml;ten 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 Variet&auml;t von <a href="glossar/glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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 ausschlie&szlig;lich <a href="glossar/glossar-m.html#c12658" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>marin </a>lebenden Kopff&uuml;&szlig;er mit mehr als 1500 bekannten Gattungen und 30 &ndash; 40 000 Arten. Sie stellen seit ihrem ersten Auftreten im Unterdevon bis zu ihrem Aussterben am Ende der Kreide eine gro&szlig;e Zahl von <a href="glossar/glossar-l.html#c12650" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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 gef&auml;rbte, st&auml;ngelige, <a href="glossar/glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>gesteinsbildende </a><a href="glossar/glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Metamorphes</a><a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gestein</a>, welches haupts&auml;chlich aus <a href="glossar.html#c12552" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Quarz</a>, <a href="glossar/glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Pyroxen</a>, <a href="glossar/glossar-g.html#c12612" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Epidot </a>k&ouml;nnen 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">&raquo;&nbsp;</span>Metamorphose </a>mit 450 &ndash; 700 &deg;C und 0,2 &ndash; 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">&raquo;&nbsp;</span>Intermedi&auml;res</a><a href="glossar/glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>vulkanisches</a><a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Plagioklas</a>, <a href="glossar/glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Pyroxen</a>, <a href="glossar/glossar-h.html#c12622" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Mineral</a>name f&uuml;r Kalzium<a href="glossar/glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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 gr&ouml;&szlig;er als der Niederschlag, sodass sich keine dauerhaften Gew&auml;sser bilden k&ouml;nnen.</p></div>
<div id="c12557" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Asthenosph&auml;re bzw. Asthenosph&auml;rischer 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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Lithosph&auml;re</a> (10 &ndash; 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 gef&auml;rbtes <a href="glossar/glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>silikatisches</a><a href="glossar/glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Kalzium</a>, Eisen und Magnesium enth&auml;lt. 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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>intermedi&auml;ren</a><a href="glossar/glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>vulkanischen</a><a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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>Ger&ouml;lle aus <a href="glossar/glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>kristallinen</a><a href="glossar/glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gesteinen</a> der Zentralalpen, auf Hochfl&auml;chen bzw. umgelagert in H&ouml;hlen der N&ouml;rdlichen Kalkalpen; <a href="glossar/glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Erosions</a>relikte einstiger Flussablagerungen aus dem Pal&auml;ogen.</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. F&uuml;r nur leicht verschobene, noch in unmittelbarer Verbindung zu ihrem Bildungsort stehende Objekte wird der Begriff parautochthon benutzt.</p></div>
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