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<input id="kesearchpagenumber" type="hidden" name="tx_kesearch_pi1[page]" value="1">
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<input id="sortByDir" type="hidden" name="tx_kesearch_pi1[sortByDir]" value="">
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</div>
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<div class="row custom-row" id="pageWrap">
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<div class="col-md-3 custom-column">
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<div id="sidebar" class="content">
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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>
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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="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>
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<div id="maincontent" class="content">
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<div id="c12985" 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 {
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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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#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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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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<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>
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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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<div class="toggle-content">
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<h1>Österreichs geologische Entwicklungsgeschichte</h1>
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