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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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Glossar
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Begriffe von A - Z
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<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">&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><a href="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-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><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">&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="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">&raquo;&nbsp;</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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Pang&auml;a</a> im Jura entstand und in der sp&auml;ten Kreide mit der durchgehenden &Ouml;ffnung 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 fr&uuml;h pal&auml;ozoischer Kontinent, der weite Teile des heutigen Nordamerika sowie Gr&ouml;nland 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 pal&auml;ozoischer 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">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Baltica</a> und <a href="glossar-l.html#c12647" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Gesteins</a>schmelze (<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>), die bei vulkanischer T&auml;tigkeit (<a href="glossar-v.html#c12753" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Vulkanismus</a>) an der Erdoberfl&auml;che 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">&raquo;&nbsp;</span>Fossil</a>, mit dem sich das relative Alter des umschlie&szlig;enden <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> ermitteln l&auml;sst; ideale Leitfossilien waren m&ouml;glichst 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">&raquo;&nbsp;</span>Gesteinen</a> nach &auml;u&szlig;eren Merkmalen. H&auml;ufig wird die mineralische (<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>) 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>Lithosph&auml;re:</h3><p>Umfasst die <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>Erdmantels</a>; ist in Platten (= Lithosph&auml;renplatten; <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>) 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>Lithosph&auml;rischer 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">&raquo;&nbsp;</span>Erdmantels</a> (10 &ndash; 200 km) mit einer Temperatur von weniger als 1300&deg; 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">&raquo;&nbsp;</span>Lithosph&auml;re</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>L&ouml;ss:</h3><p>Windverfrachtetes, feink&ouml;rniges, ungeschichtetes <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sediment</a>, das w&auml;hrend Kaltzeiten (<a href="glossar-g.html#c12606" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</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">&raquo;&nbsp;</span>kalk</a>ige Verkittung gegebene Standfestigkeit (Hohlwege, Weinkeller).</p></div>
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