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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 &bdquo;Reichtum Erde&ldquo; von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. &copy; Geosphere Austria
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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 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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<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>
Glossar
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Begriffe von A - Z
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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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&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-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-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-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-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-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-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-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-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-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-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-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Plutonisches</a><a href="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-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Plagioklas</a> und <a href="glossar-p.html#c12702" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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 (&bdquo;Gang&ldquo;) eingedrungene und kristallisierte (<a href="glossar-k.html#c12645" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Kristallin</a>) Gesteinsschmelze (<a href="glossar-m.html#c12438" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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, haupts&auml;chlich durch Prozesse der <a href="glossar-p.html#c12695" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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>Gef&uuml;gekunde:</h3><p>Lehre von der Analyse und Interpretation der r&auml;umlichen Anordnung der <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Kl&uuml;fte</a>, Schieferungsfl&auml;chen (<a href="glossar-s.html#c12719" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Gesteins</a>k&ouml;rper.</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 nat&uuml;rlichen radioaktiven Isotopen (<a href="glossar-r.html#c12704" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Gesteinen</a> die sie aufbauen und den physikalischen, chemischen und biologischen Ver&auml;nderungen 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 Oberfl&auml;che 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, gr&ouml;&szlig;ere <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gesteins</a>st&uuml;cke, die beim Eistransport einer charakteristischen Oberfl&auml;chenbearbeitung unterliegen. Wenn Geschiebe Ritzer und Schrammen aufweisen, werden sie als &bdquo;gekritzte Geschiebe&ldquo; bezeichnet.&nbsp; </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, vielk&ouml;rniges <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Mineral</a>aggregat, relativ selten auch nat&uuml;rliches Glas oder R&uuml;ckstand von Organismen. Gesteine treten in selbstst&auml;ndigen, zusammenh&auml;ngenden, <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>geologisch</a> kartierbaren K&ouml;rpern 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">&raquo;&nbsp;</span>Minerale</a>, die in gen&uuml;gender Menge und H&auml;ufi gkeit vorhanden sind, um <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Silikate</a>, <a href="glossar-k.html#c12629" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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> &sdot; 2 H<sub>2</sub>O); wei&szlig; oder r&ouml;tlich gef&auml;rbtes <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Mineral</a> mit geringer H&auml;rte, in <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sedimentgesteinen</a> auch <a href="glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Gesteinsbildende </a>Schicht<a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>silikate</a> mit bl&auml;ttchenf&ouml;rmiger <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Biotit</a> und <a href="glossar-m.html#c12675" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Quarz</a> und <a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Feldspat</a>. Bei gr&ouml;&szlig;erem Gehalt an <a href="glossar-g.html#c12612" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Quarz</a> und <a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Feldspat</a> sind, wobei &gt; 20 % Feldspat und &lt; 50 % <a href="glossar-g.html#c12607" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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>Pal&auml;ozoischer Gro&szlig;kontinent, in dem die alten Kerne der heutigen Kontinente S&uuml;damerika, 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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Schichtfolge</a>, benannt nach der Ortschaft Gosau (O.&Ouml;.), mit gro&szlig;teils <a href="glossar-m.html#c12658" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>marinen</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sedimenten</a> aus der sp&auml;ten Kreide bis ins Pal&auml;ogen. Diese wurde w&auml;hrend der <a href="../glossar.html#c12549" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>&Uuml;berschiebung</a> von <a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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>R&ouml;tlich gef&auml;rbte <a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>silikatische</a><a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Minerale</a> mit ann&auml;hernd kugelf&ouml;rmiger <a href="glossar-k.html#c12644" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Kristallform</a>; <a href="glossar-g.html#c12604" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>gesteinsbildend</a> in <a href="glossar-g.html#c12608" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Glimmerschiefer</a> und <a href="glossar-g.html#c12609" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Quarz</a>, Alkali<a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>feldspat</a> und <a href="glossar-p.html#c12693" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Plagioklas</a> besteht, gew&ouml;hnlich mit <a href="glossar-b.html#c12755" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>gestein</a> als <a href="glossar-g.html#c12613" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gestein</a>, das unter sehr hohen Temperaturbedingungen bei 700 &ndash; 1 000 &deg;C und 0,4 &ndash; 1,8 GPa Druck gebildet wurde. Granulit enth&auml;lt kaum noch <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Mineral</a>, <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</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 gr&uuml;nlicher <a href="glossar-s.html#c12711" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Sand</a>komponenten &uuml;berwiegt <a href="glossar-q.html#c12462" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Quarz</a> gegen&uuml;ber h&auml;ufi gen <a href="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;cken.</p></div>
<div id="c12619" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Grundmor&auml;ne:</h3><p>An der Basis des Gletschereises gebildete Ablagerung, die sehr dicht gelagert ist und gro&szlig;teils aus feink&ouml;rnig zerriebenem <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gesteins</a>material mit einzelnen gr&ouml;beren Komponenten (<a href="glossar-g.html#c12602" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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>Gr&uuml;nschiefer:</h3><p><a href="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-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gestein</a>, dessen gr&uuml;nliche Farbe sich von <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Mineralen</a> wie <a href="../glossar.html#c12552" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Amphibol</a>, <a href="glossar-c.html#c12571" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Chlorit</a> und <a href="glossar-e.html#c12582" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>basischem</a><a href="glossar-v.html#c12754" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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>Gr&uuml;nschieferfazies:</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">&raquo;&nbsp;</span>Metamorphose</a> zwischen 300 &ndash; 450 &deg;C und 0,1 &ndash; 0,8 GPa Druck.</p></div>
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