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<h1 id="firstHeading" class="firstHeading mw-first-heading"><span class="mw-page-title-main">Ganges Chasma</span></h1>
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<div id="mw-content-text" class="mw-body-content mw-content-ltr" lang="de" dir="ltr"><div class="mw-content-ltr mw-parser-output" lang="de" dir="ltr"><table class="wikitable infobox float-right" id="infobox_außerirdische_region" style="font-size:90%; min-width:15%; width:310px; max-width:47%;">
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<th colspan="2" style="background:#C0C0C0; color:#202122; font-size:larger;">Grabenbruch auf dem <a href="Mars_(Planet)" title="Mars (Planet)">Mars</a>
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<th colspan="2" style="background:#DCDCDC; color:#202122;">Ganges Chasma
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<td colspan="2" style="background:#000000; color::inherit; text-align:center;"><span typeof="mw:File"></span>
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<td colspan="2" style="text-align:center;">Links: eine Klippe am Nordrand, auf einer Aufnahme von <a href="THEMIS" title="THEMIS">THEMIS</a>; rechts: topografische Übersicht mit linkem Ausschnitt in rotem Rahmen
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<td>Position
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<td nowrap=""><span id="Ganges_Chasma" class="coordinates -print"><a class="external text" href="geo:-8,-48.016666666667"><span title="Breitengrad">8° <abbr title="Süd">S</abbr></span>, <span title="Längengrad">48° <abbr title="West">W</abbr></span></a></span><span class="geo noexcerpt" style="display:none"><span class="body">Mars</span><span class="latitude">-8</span><span class="longitude">-48.016666666667</span><span class="elevation"></span></span>
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<td>Ausdehnung
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<td nowrap="">584 km
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<td>Region
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<td nowrap=""><a href="Xanthe_Terra" title="Xanthe Terra">Xanthe Terra</a>
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<td colspan="2" style="background:#DCDCDC; color:#202122;"><b>Geschichte</b>
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<td>Benannt nach
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<td nowrap=""><a href="Ganges" title="Ganges">Ganges</a>
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<p><b>Ganges Chasma</b> ist ein tiefer <a href="Canyon" title="Canyon">Canyon</a> auf dem <a href="Mars_(Planet)" title="Mars (Planet)">Mars</a>. Er wurde 1973 nach dem <a href="Ganges" title="Ganges">Ganges</a> in Südasien benannt.<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup>
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<div class="mw-heading mw-heading2"><h2 id="Beschreibung">Beschreibung</h2></div>
<p>Ganges Chasma befindet sich im Süden des Hochlands <a href="Xanthe_Terra" title="Xanthe Terra">Xanthe Terra</a>, am östlichen Ende des ausgedehnten Systems der <a href="Vallis_Marineris" class="mw-redirect" title="Vallis Marineris">Vallis Marineris</a>. Die Schlucht ist 584 km lang und enthält die 136 km weite Hochfläche Ganges Mensa.<sup id="cite_ref-2" class="reference"><a href="#cite_note-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup> Im Osten des <a href="Chasma" title="Chasma">Chasma</a> schließt sich Capri Chasma an. Es wird davon ausgegangen, dass sich Ganges Chasma durch eine Abfolge großer Ausflüsse von Wasser und CO<sub>2</sub> aus <a href="Chaotisches_Terrain" title="Chaotisches Terrain">chaotischen Terrain</a> wie Ganges Chaos im Süden gebildet hat.<sup id="cite_ref-RodriguezKargel2006_3-0" class="reference"><a href="#cite_note-RodriguezKargel2006-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup> Zusätzlich wird davon ausgegangen, dass die meisten Hinweise darauf ausgewaschen wurden.<sup id="cite_ref-RodriguezKargel2006_3-1" class="reference"><a href="#cite_note-RodriguezKargel2006-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup> Zuerst entwickelte sich ein Ausläufer, der sich mit Capri Chasma und den verbundenen Ausflusskanälen im Osten verband. Zwischenzeitlich, während der <a href="Mars_(Planet)#Noachische_Periode" title="Mars (Planet)">Noachischen Periode</a>, bestand möglicherweise ein See mit Abfluss nach Norden, teilweise unterirdisch im <a href="Shalbatana_Vallis" title="Shalbatana Vallis">Shalbatana Vallis</a>.<sup id="cite_ref-Rodriguez2003_4-0" class="reference"><a href="#cite_note-Rodriguez2003-4"><span class="cite-bracket">[</span>4<span class="cite-bracket">]</span></a></sup>
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<div class="mw-heading mw-heading2"><h2 id="Detailgalerie">Detailgalerie</h2></div>
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<div class="gallerytext">Helle, erodiertere Ablagerungen auf dunkleren Schichten</div>
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<li class="gallerybox" style="width: 155px">
<div class="thumb" style="width: 150px; height: 150px;"><span typeof="mw:File"></span></div>
<div class="gallerytext">Sedimentschichten am oberen Hang in höherer Bildauflösung</div>
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<li class="gallerybox" style="width: 155px">
<div class="thumb" style="width: 150px; height: 150px;"><span typeof="mw:File"></span></div>
<div class="gallerytext">Erdrutsch am Nordwesthang</div>
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<li class="gallerybox" style="width: 155px">
<div class="thumb" style="width: 150px; height: 150px;"><span typeof="mw:File"></span></div>
<div class="gallerytext"><a href="Kleintrombe" title="Kleintrombe">„Staubteufel“</a> im Ganges Chasma</div>
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<div class="mw-heading mw-heading2"><h2 id="Einzelnachweise">Einzelnachweise</h2></div>
<ol class="references">
<li id="cite_note-1"><span class="mw-cite-backlink"><a href="#cite_ref-1">↑</a></span> <span class="reference-text"><a rel="nofollow" class="external text" href="https://planetarynames.wr.usgs.gov/Feature/2096">Ganges Chasma</a> im <i>Gazetteer of Planetary Nomenclature</i> der <a href="Internationale_Astronomische_Union" title="Internationale Astronomische Union">IAU</a> (WGPSN) / <a href="United_States_Geological_Survey" title="United States Geological Survey">USGS</a></span>
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<li id="cite_note-2"><span class="mw-cite-backlink"><a href="#cite_ref-2">↑</a></span> <span class="reference-text"><a rel="nofollow" class="external text" href="https://planetarynames.wr.usgs.gov/Feature/2097">Ganges Mensa</a> im <i>Gazetteer of Planetary Nomenclature</i> der <a href="Internationale_Astronomische_Union" title="Internationale Astronomische Union">IAU</a> (WGPSN) / <a href="United_States_Geological_Survey" title="United States Geological Survey">USGS</a></span>
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<li id="cite_note-RodriguezKargel2006-3"><span class="mw-cite-backlink">↑ <sup><a href="#cite_ref-RodriguezKargel2006_3-0">a</a></sup> <sup><a href="#cite_ref-RodriguezKargel2006_3-1">b</a></sup></span> <span class="reference-text">J. A. P. Rodriguez, J. Kargel, D. A. Crown, L. F. Bleamaster, K. L. Tanaka, V. Baker, H. Miyamoto, J. M. Dohm, S. Sasaki, G. Komatsu: <cite style="font-style:italic">Headward growth of chasmata by volatile outbursts, collapse, and drainage: Evidence from Ganges chaos, Mars</cite>. In: <cite style="font-style:italic">Geophysical Research Letters</cite>. 33. Jahrgang, <span style="white-space:nowrap">Nr.<span style="display:inline-block;width:.2em"> </span>18</span>, September 2006, <a href="Internationale_Standardnummer_f%C3%BCr_fortlaufende_Sammelwerke" title="Internationale Standardnummer für fortlaufende Sammelwerke">ISSN</a> <span style="white-space:nowrap"><a rel="nofollow" class="external text" href="https://zdb-katalog.de/list.xhtml?t=iss%3D%220094-8276%22&key=cql">0094-8276</a></span>, <a href="Digital_Object_Identifier" title="Digital Object Identifier">doi</a>:<span class="uri-handle" style="white-space:nowrap"><a rel="nofollow" class="external text" href="https://doi.org/10.1029/2006GL026275">10.1029/2006GL026275</a></span>.<span class="Z3988" title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rfr_id=info:sid/de.wikipedia.org:Ganges+Chasma&rft.atitle=Headward+growth+of+chasmata+by+volatile+outbursts%2C+collapse%2C+and+drainage%3A+Evidence+from+Ganges+chaos%2C+Mars&rft.au=J.+A.+P.%26%2332%3BRodriguez%2C%26%2332%3BJ.%26%2332%3BKargel%2C%26%2332%3BD.+A.%26%2332%3BCrown%2C+...&rft.date=2006-09&rft.doi=10.1029%2F2006GL026275&rft.genre=journal&rft.issn=0094-8276&rft.issue=18&rft.jtitle=Geophysical+Research+Letters&rft.volume=33.+Jahrgang" style="display:none"> </span></span>
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<li id="cite_note-Rodriguez2003-4"><span class="mw-cite-backlink"><a href="#cite_ref-Rodriguez2003_4-0">↑</a></span> <span class="reference-text">J. A. P. Rodriguez, S. Sasaki, H. Miyamoto: <cite style="font-style:italic">Nature and hydrological relevance of the Shalbatana complex underground cavernous system</cite>. In: <cite style="font-style:italic">Geophysical Research Letters</cite>. 30. Jahrgang, <span style="white-space:nowrap">Nr.<span style="display:inline-block;width:.2em"> </span>6</span>, 2003, <a href="Internationale_Standardnummer_f%C3%BCr_fortlaufende_Sammelwerke" title="Internationale Standardnummer für fortlaufende Sammelwerke">ISSN</a> <span style="white-space:nowrap"><a rel="nofollow" class="external text" href="https://zdb-katalog.de/list.xhtml?t=iss%3D%220094-8276%22&key=cql">0094-8276</a></span>, <a href="Digital_Object_Identifier" title="Digital Object Identifier">doi</a>:<span class="uri-handle" style="white-space:nowrap"><a rel="nofollow" class="external text" href="https://doi.org/10.1029/2002GL016547">10.1029/2002GL016547</a></span>.<span class="Z3988" title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rfr_id=info:sid/de.wikipedia.org:Ganges+Chasma&rft.atitle=Nature+and+hydrological+relevance+of+the+Shalbatana+complex+underground+cavernous+system&rft.au=J.+A.+P.%26%2332%3BRodriguez%2C%26%2332%3BS.%26%2332%3BSasaki%2C%26%2332%3BH.%26%2332%3BMiyamoto&rft.date=2003&rft.doi=10.1029%2F2002GL016547&rft.genre=journal&rft.issn=0094-8276&rft.issue=6&rft.jtitle=Geophysical+Research+Letters&rft.volume=30.+Jahrgang" style="display:none"> </span></span>
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