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<h1 id="firstHeading" class="firstHeading mw-first-heading"><span class="mw-page-title-main">Mount Siple</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 toptextcells float-right" id="Vorlage-Infobox-Berg" summary="Infobox Berg" style="margin-top:0; font-size:95%; width:310px;">
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<th colspan="2" style="background:#E7DCC3; color:#202122; font-size:125%;">Mount Siple
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<td colspan="2" style="text-align:center; padding:2px; border-bottom:0;"><span typeof="mw:File"></span>
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<td colspan="2" style="text-align:center; padding:2px; border-top:0;">Topografische Karte vom Mount Siple
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<td><a href="H%C3%B6he_%C3%BCber_dem_Meeresspiegel" title="Höhe über dem Meeresspiegel">Höhe</a>
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<td><span style="border-width:0px; padding:0px; margin:0px;">3110 <abbr title="Höhe über dem Meeresspiegel">m</abbr></span>
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<td>Lage
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<td><a href="Siple-Insel" title="Siple-Insel">Siple-Insel</a>, <a href="Antarktis" title="Antarktis">Antarktis</a>
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<td><a href="Dominanz_(Geographie)" title="Dominanz (Geographie)">Dominanz</a>
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<td>363 km<span title="zum Berg"> → </span><a href="Mount_Hampton" title="Mount Hampton">Mount Hampton</a>
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<td><a href="Schartenh%C3%B6he" title="Schartenhöhe">Schartenhöhe</a>
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<td>3110 m
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<td><a href="World_Geodetic_System_1984" title="World Geodetic System 1984">Koordinaten</a>
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<td><span id="text_coordinates" class="coordinates -print"><a class="external text" href="geo:-73.433333333333,-126.66666666667"><span title="Breitengrad">73° 26′ 0″ <abbr title="Süd">S</abbr></span>, <span title="Längengrad">126° 40′ 0″ <abbr title="West">W</abbr></span></a></span><span class="geo noexcerpt" style="display:none"><span class="body"></span><span class="latitude">-73.433333333333</span><span class="longitude">-126.66666666667</span><span class="elevation">3110</span></span>
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<td>Typ
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<td><a href="Schildvulkan" title="Schildvulkan">Schildvulkan</a>, gegenwärtig inaktiv
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<td><a href="Erstbesteigung" title="Erstbesteigung">Erstbesteigung</a>
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<td>unbestiegen
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<td colspan="2" style="text-align:center; padding:2px; border-bottom:0;"><span typeof="mw:File"></span>
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<td colspan="2" style="text-align:center; padding:2px; border-top:0;">Luftaufnahme des Mount Siple
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</tbody></table><div style="display:none">pd3</div><div style="display:none">pd5</div><div style="display:none">fd2</div><div style="display:none">Vorlage:Infobox Berg/Wartung/BILD1</div><div class="editoronly" style="display:none;"></div>
<p>Der <b>Mount Siple</b> ist ein gegenwärtig inaktiver <a href="Schildvulkan" title="Schildvulkan">Schildvulkan</a> in der <a href="Antarktis" title="Antarktis">Antarktis</a>.
</p><p>Der 3110 m hohe Vulkan ist ein ausgedehnter schneebedeckter Berg mit einem kegelförmigen Bau und einer im Durchmesser fünf Kilometer weiten <a href="Caldera_(Krater)" title="Caldera (Krater)">Gipfelcaldera</a>. Er dominiert den nordwestlichen Teil der <a href="Siple-Insel" title="Siple-Insel">Siple-Insel</a>, die durch das <a href="Getz-Schelfeis" title="Getz-Schelfeis">Getz-Schelfeis</a> von der <a href="Bakutis-K%C3%BCste" title="Bakutis-Küste">Bakutis-Küste</a> getrennt ist.
</p><p>Der Vulkan mit einem Gesteinsvolumen von rund 1800 km³ entstand während der letzten 2 Mio. Jahre, einige seiner <a href="Flankenvulkan" title="Flankenvulkan">Flankenvulkane</a> sind jünger als 100.000 Jahre.<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> Ausbrüche während des <a href="Holoz%C3%A4n" title="Holozän">Holozäns</a> gelten als wahrscheinlich. In den Jahren 1988 und 2012 glaubte man, auf Satellitenaufnahmen Anzeichen von Asche- und Dampfwolken zu erkennen; weitere Untersuchungen erbrachten allerdings keine Hinweise auf einen aktuellen Ausbruch.
</p><p>Der Berg trägt den Namen von <a href="Paul_Siple" title="Paul Siple">Paul Allman Siple</a> (1908–1968), einem US-amerikanischen Antarktisforscher und Geografen, der an sechs Antarktisexpeditionen teilnahm, unter anderem an den ersten beiden Expeditionen von <a href="Richard_Evelyn_Byrd" title="Richard Evelyn Byrd">Richard Evelyn Byrd</a> zur <a href="Siple-K%C3%BCste" title="Siple-Küste">Siple-Küste</a> (1928–1930) und zur Siple-Insel (1933–1935). Der Berg wurde während eines Erkundungsfluges entdeckt, bei dem Siple als <a href="Navigator" title="Navigator">Navigator</a> diente.
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<div class="mw-heading mw-heading2"><h2 id="Weblinks">Weblinks</h2></div>
<ul><li><a rel="nofollow" class="external text" href="https://volcano.si.edu/volcano.cfm?vn=390025"><i>Siple</i></a> im <i>Global Volcanism Program</i> der <a href="Smithsonian_Institution" title="Smithsonian Institution">Smithsonian Institution</a> (englisch).</li>
<li><a rel="nofollow" class="external text" href="http://www.skimountaineer.com/ROF/ROF.php?name=Siple"><i>Skiing the Pacific Ring of Fire and Beyond: Mount Siple.</i></a> In: <i>skimountaineer.com.</i> Amar Andalkar (englisch).</li>
<li><span class="cite"><a rel="nofollow" class="external text" href="https://web.archive.org/web/2020/https://geonames.usgs.gov/apex/f?p=gnispq:5:::NO::P5_ANTAR_ID:13879"><i>Mount Siple.</i></a> In: <i><a href="Geographic_Names_Information_System" title="Geographic Names Information System">Geographic Names Information System</a>.</i> <a href="United_States_Geological_Survey" title="United States Geological Survey">United States Geological Survey</a>, <a href="United_States_Department_of_the_Interior" class="mw-redirect" title="United States Department of the Interior">United States Department of the Interior</a>, archiviert vom <style data-mw-deduplicate="TemplateStyles:r250917974">
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<div class="mw-heading mw-heading2"><h2 id="Einzelnachweise">Einzelnachweise</h2></div>
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<li id="cite_note-1"><span class="mw-cite-backlink"><a href="#cite_ref-1">↑</a></span> <span class="reference-text"><span class="cite">Lucia Sala Simian: <a rel="nofollow" class="external text" href="https://web.archive.org/web/20170407140850/http://www.anta.canterbury.ac.nz/documents/GCAS_7/Simion_L_Lit.Review.pdf#page=16"><i>Literature Review (Anta 502): The volcanoes of Marie Byrd Land and their importance in understanding the tectonics of West Antarctica as well as the reconstruction of the West Antarctic ice sheet (WAIS) in the last interglacial.</i></a> (PDF; 123 kB) Graduate Course in Antarctic Studies 2004–2005. <a href="University_of_Canterbury" title="University of Canterbury">University of Canterbury</a>, 10. Januar 2005, archiviert vom <span class="dewiki-iconexternal"><a class="external text" href="https://redirecter.toolforge.org/?url=http%3A%2F%2Fwww.anta.canterbury.ac.nz%2Fdocuments%2FGCAS_7%2FSimion_L_Lit.Review.pdf%23page%3D16">Original</a></span> (nicht mehr online verfügbar) am <span style="white-space:nowrap;">7. April 2017</span><span>;</span><span class="Abrufdatum"> abgerufen am 24. August 2017</span> (englisch).</span> <small class="archiv-bot"><span class="wp_boppel noviewer" aria-hidden="true" role="presentation"><span typeof="mw:File"><span title="i"></span></span></span> <b>Info:</b> Der Archivlink wurde automatisch eingesetzt und noch nicht geprüft. Bitte prüfe Original- und Archivlink gemäß Anleitung und entferne dann diesen Hinweis.</small><span style="display:none"><a rel="nofollow" class="external text" href="http://IABotmemento.invalid/http://www.anta.canterbury.ac.nz/documents/GCAS_7/Simion_L_Lit.Review.pdf#page=16">@1</a></span><span style="display:none"><a rel="nofollow" class="external text" href="http://www.anta.canterbury.ac.nz/documents/GCAS_7/Simion_L_Lit.Review.pdf#page=16">@2</a></span><span style="display:none">Vorlage:Webachiv/IABot/www.anta.canterbury.ac.nz</span><span style="display: none;" class="Z3988" title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2Fde.wikipedia.org%3AMount+Siple&rft.title=Literature+Review+%28Anta+502%29%3A+The+volcanoes+of+Marie+Byrd+Land+and+their+importance+in+understanding+the+tectonics+of+West+Antarctica+as+well+as+the+reconstruction+of+the+West+Antarctic+ice+sheet+%28WAIS%29+in+the+last+interglacial&rft.description=Literature+Review+%28Anta+502%29%3A+The+volcanoes+of+Marie+Byrd+Land+and+their+importance+in+understanding+the+tectonics+of+West+Antarctica+as+well+as+the+reconstruction+of+the+West+Antarctic+ice+sheet+%28WAIS%29+in+the+last+interglacial&rft.identifier=https%3A%2F%2Fweb.archive.org%2Fweb%2F20170407140850%2Fhttp%3A%2F%2Fwww.anta.canterbury.ac.nz%2Fdocuments%2FGCAS_7%2FSimion_L_Lit.Review.pdf%23page%3D16&rft.creator=Lucia+Sala+Simian&rft.publisher=%5B%5B+University+of+Canterbury%5D%5D&rft.date=2005-01-10&rft.source=http://www.anta.canterbury.ac.nz/documents/GCAS_7/Simion_L_Lit.Review.pdf#page=16&rft.language=en"> </span></span>
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