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href="http://dbpedia.org/resource/Wilkins_Sound">Wilkins Sound</a> </h1> </div> </div> <div class="row"> <div class="col"> <div class="text-muted"> An Entity of Type: <a href="http://dbpedia.org/ontology/Island">island</a>, from Named Graph: <a href="http://dbpedia.org">http://dbpedia.org</a>, within Data Space: <a href="http://dbpedia.org">dbpedia.org</a> </div> </div> </div> <div class="row pt-2"> <div class="col-xs-9 col-sm-10"> Wilkins Sound is a seaway in Antarctica that is largely occupied by the Wilkins Ice Shelf. It is located on the southwest side of the Antarctic Peninsula between the concave western coastline of Alexander Island and the shores of Charcot Island and Latady Island farther to the west. </div> <div class="col-xs-3 col-sm-2"> <a href="#" class="thumbnail"> <img src="http://commons.wikimedia.org/wiki/Special:FilePath/Ant-pen_map.png?width=300" alt="thumbnail" class="img-fluid" /> </a> </div> </div> </div> </section>   <section> <div class="container-xl"> <div class="row"> <div class="table-responsive"> <table class="table table-hover table-sm table-light"> <thead> <tr> <th class="col-xs-3 ">Property</th> <th class="col-xs-9 px-3">Value</th> </tr> </thead> <tbody> <tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/abstract">dbo:abstract</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">L'estret de Wilkins (oficialment, en anglès, Wilkins Sound) és un estret de l'Antàrtida que està ocupat en gran part per la plataforma de gel Wilkins; està situat entre la concava línia de costa occidental de l' i les costes de l'illa Charcot i l' situades més cap a l'oest. La seva part nord va ser descoberta i cartografiada aproximadament el 1910 per una expedició antàrtica francesa sota el comandament de Jean-Baptiste Charcot i es va sobrevolar el 1929 per . La configuració de l'estret fou determinada el 1940 mitjançant vols exploratoris del (USAS). Fou anomenat així per l'USAS en honor d'Hubert Wilkins, que el 1929 fou el primer a demostrar que "la terra de Charcot" era en realitat una illa i era per tant, indirectament, el descobridor de l'existència de l'estret. L'existència de l'illa Latady en el costat sud-oest de l'estret fou determinada el 1960 per D.J.H. Searle del Falkland Islands Dependencies Survey (FIDS) mitjançant l'examen de fotos aèries fetes per la (RAR) del 1947-48. (ca)</li> <li style="display:none;">Der Wilkins-Sund ist eine größtenteils vom Wilkins-Schelfeis besetzte Meerenge in der antarktischen Bellingshausen-See. Sie liegt zwischen der westlichen Küstenlinie der Alexander-I.-Insel und der vorgelagerten Charcot- und der Latady-Insel. Der nördliche Teil des Sunds wurde 1910 von Teilnehmern der Fünften Französischen Antarktisexpedition (1908–1910) unter der Leitung des Polarforschers Jean-Baptiste Charcot erstmals gesichtet und grob kartiert. Der australische Polarforscher Hubert Wilkins, Namensgeber des Sunds, überflog ihn im Jahr 1929. Wissenschaftler der United States Antarctic Service Expedition (1939–1941) ermittelten 1940 seine Ausdehnung und nahmen die Benennung vor. Der britische Geograph Derek Searle kartierte ihn gemeinsam mit der Latady-Insel anhand von Luftaufnahmen der US-amerikanischen Ronne Antarctic Research Expedition (1947–1948). (de)</li> <li style="display:none;">Wilkins-bankizo en Antarkto estas bankizo (glacia "karapaco") flosanta sur la malprofunda maro.Ĝi vastas 13.000 km² kaj situas vidalvide de Fajrolando, en distanco de 1.600 km al la suda pinto de Sudameriko. Wilkins-bankizo ricevis publikan atenton en marto 2008, kiam granda parto de la glacio forrompiĝis Kiel kaŭzon sciencistoj supozas la fandiĝon de la glacio pro la tutmonda varmiĝo, kiu aparte trafas la regionon de Antarkto. (eo)</li> <li style="display:none;">Le détroit de Wilkins (anglais : Wilkins Sound) est un détroit du sud-ouest de la péninsule Antarctique, en Antarctique. Plus précisément, il se trouve à l'ouest de l'île Alexandre-Ier. Il est occupé largement par la barrière de Wilkins. Sa partie nord fut cartographiée en 1910 durant la seconde expédition Charcot dirigées par Jean-Baptiste Charcot. Elle fut observée de manière aérienne en 1929 par Hubert Wilkins. Le 5 avril 2009, le mince pont de glace naturel reliant la barrière de Wilkins au continent s'est scindé, ce qui pourrait entraîner, selon des scientifiques, à un effondrement de la barrière. On rapporte également que la barrière se désintègre en centaines de petits morceaux de glace. Selon David Vaughan du British Antarctic Survey, ceci serait dû au réchauffement climatique. (fr)</li> <li>Wilkins Sound is a seaway in Antarctica that is largely occupied by the Wilkins Ice Shelf. It is located on the southwest side of the Antarctic Peninsula between the concave western coastline of Alexander Island and the shores of Charcot Island and Latady Island farther to the west. Its northern portion was first seen and roughly mapped in 1910 by the French Antarctic Expedition under Jean-Baptiste Charcot and was observed from the air in 1929 by Sir Hubert Wilkins. The configuration of the sound was determined in 1940 on exploratory flights by the US Antarctic Service (USAS). It was named by the USAS for Sir Hubert Wilkins, who in 1929 first proved "Charcot Land" to be an island (see Charcot Island) and thereby indirectly discovered this feature. The existence of Latady Island at the southwest side of the sound was determined in 1960 by D.J.H. Searle of Falkland Islands Dependencies Survey (FIDS) by examination of air photos taken by the Ronne Antarctic Research Expedition (RARE), 1947–48. On 5 April 2009 the thin bridge of ice to the Wilkins Ice Shelf off the coast of Antarctica splintered, and scientists expect it could cause the collapse of the Shelf. There are reports the shelf has exploded into hundreds of small icebergs. David Vaughan of the British Antarctic Survey has attributed these events to global warming. (en)</li> <li style="display:none;">Wilkins är en strömfåra i Antarktis. Den ligger i Västantarktis. Argentina, Chile och Storbritannien gör anspråk på området. (sv)</li> <li style="display:none;">威爾金斯冰架（英語：Wilkins Sound）位處南極洲西部南極半島一個面積為130公里乘110公里的冰架，名字是由UK-APC （页面存档备份，存于互联网档案馆）於1971年改的。在1993年，(BAS)教授David Vaughan 預計，若南極洲以這個速度暖化，威爾金斯冰架北部將於30年內消失。自2008年2月28日，威爾金斯冰架已經開始斷裂。於3月25日，美國科學家借助衛星圖像證實，南極半島的一塊巨大冰川從威爾金斯冰架邊緣斷裂入海，面積大約是415平方公里，反映全球暖化問題進一步惡化。科學家們發現，餘下14,000平方公里的冰架也開始斷裂入海。冰架現時只有一條狹窄的薄冰與南極半島相連。此次冰架斷裂，臺灣成功大學及國家太空中心亦利用福爾摩沙衛星二號參與拍攝，並於3月8日獲得關鍵影像。 (zh)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/country">dbo:country</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="dbo:country" resource="http://dbpedia.org/resource/Antarctica" href="http://dbpedia.org/resource/Antarctica">dbr:Antarctica</a></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/location">dbo:location</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="dbo:location" resource="http://dbpedia.org/resource/Antarctica" 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href="http://dbpedia.org/class/yago/YagoPermanentlyLocatedEntity">yago:YagoPermanentlyLocatedEntity</a></li> <li><a class="uri" rel="rdf:type" resource="http://dbpedia.org/class/yago/Strait109446115" href="http://dbpedia.org/class/yago/Strait109446115">yago:Strait109446115</a></li> <li><a class="uri" rel="rdf:type" resource="http://dbpedia.org/class/yago/Thing100002452" href="http://dbpedia.org/class/yago/Thing100002452">yago:Thing100002452</a></li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#comment">rdfs:comment</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">Wilkins-bankizo en Antarkto estas bankizo (glacia "karapaco") flosanta sur la malprofunda maro.Ĝi vastas 13.000 km² kaj situas vidalvide de Fajrolando, en distanco de 1.600 km al la suda pinto de Sudameriko. Wilkins-bankizo ricevis publikan atenton en marto 2008, kiam granda parto de la glacio forrompiĝis Kiel kaŭzon sciencistoj supozas la fandiĝon de la glacio pro la tutmonda varmiĝo, kiu aparte trafas la regionon de Antarkto. (eo)</li> <li style="display:none;">Wilkins är en strömfåra i Antarktis. Den ligger i Västantarktis. Argentina, Chile och Storbritannien gör anspråk på området. (sv)</li> <li style="display:none;">威爾金斯冰架（英語：Wilkins Sound）位處南極洲西部南極半島一個面積為130公里乘110公里的冰架，名字是由UK-APC （页面存档备份，存于互联网档案馆）於1971年改的。在1993年，(BAS)教授David Vaughan 預計，若南極洲以這個速度暖化，威爾金斯冰架北部將於30年內消失。自2008年2月28日，威爾金斯冰架已經開始斷裂。於3月25日，美國科學家借助衛星圖像證實，南極半島的一塊巨大冰川從威爾金斯冰架邊緣斷裂入海，面積大約是415平方公里，反映全球暖化問題進一步惡化。科學家們發現，餘下14,000平方公里的冰架也開始斷裂入海。冰架現時只有一條狹窄的薄冰與南極半島相連。此次冰架斷裂，臺灣成功大學及國家太空中心亦利用福爾摩沙衛星二號參與拍攝，並於3月8日獲得關鍵影像。 (zh)</li> <li style="display:none;">L'estret de Wilkins (oficialment, en anglès, Wilkins Sound) és un estret de l'Antàrtida que està ocupat en gran part per la plataforma de gel Wilkins; està situat entre la concava línia de costa occidental de l' i les costes de l'illa Charcot i l' situades més cap a l'oest. (ca)</li> <li style="display:none;">Der Wilkins-Sund ist eine größtenteils vom Wilkins-Schelfeis besetzte Meerenge in der antarktischen Bellingshausen-See. Sie liegt zwischen der westlichen Küstenlinie der Alexander-I.-Insel und der vorgelagerten Charcot- und der Latady-Insel. (de)</li> <li style="display:none;">Le détroit de Wilkins (anglais : Wilkins Sound) est un détroit du sud-ouest de la péninsule Antarctique, en Antarctique. Plus précisément, il se trouve à l'ouest de l'île Alexandre-Ier. Il est occupé largement par la barrière de Wilkins. Sa partie nord fut cartographiée en 1910 durant la seconde expédition Charcot dirigées par Jean-Baptiste Charcot. Elle fut observée de manière aérienne en 1929 par Hubert Wilkins. (fr)</li> <li>Wilkins Sound is a seaway in Antarctica that is largely occupied by the Wilkins Ice Shelf. It is located on the southwest side of the Antarctic Peninsula between the concave western coastline of Alexander Island and the shores of Charcot Island and Latady Island farther to the west. (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#label">rdfs:label</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">Estret de Wilkins (ca)</li> <li style="display:none;">Wilkins-Sund (de)</li> <li style="display:none;">Wilkins-bankizo (eo)</li> <li style="display:none;">Détroit de Wilkins (Antarctique) (fr)</li> <li>Wilkins Sound (en)</li> <li style="display:none;">Wilkins Sound (sv)</li> <li style="display:none;">威尔金斯冰架 (zh)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://www.w3.org/2002/07/owl#sameAs">owl:sameAs</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="owl:sameAs" resource="http://rdf.freebase.com/ns/m.0844hg" href="http://rdf.freebase.com/ns/m.0844hg">freebase:Wilkins Sound</a></li> <li><a class="uri" rel="owl:sameAs" resource="http://commons.dbpedia.org/resource/Wilkins_Sound" 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href="http://en.wikipedia.org/wiki/Wilkins_Sound">wikipedia-en:Wilkins_Sound</a></li> </ul></td></tr> </tbody> </table> </div> </div> </div> </section>   <section> <div class="container-xl"> <div class="text-center p-4 bg-light"> <a href="https://virtuoso.openlinksw.com/" title="OpenLink Virtuoso"><img class="powered_by" src="/statics/images/virt_power_no_border.png" alt="Powered by OpenLink Virtuoso"/></a>    <a href="http://linkeddata.org/"><img alt="This material is Open Knowledge" src="/statics/images/LoDLogo.gif"/></a>     <a href="http://dbpedia.org/sparql"><img alt="W3C Semantic Web Technology" src="/statics/images/sw-sparql-blue.png"/></a>     <a href="https://opendefinition.org/"><img alt="This material is Open Knowledge" src="/statics/images/od_80x15_red_green.png"/></a>    <a href="https://validator.w3.org/check?uri=referer"> <img src="https://www.w3.org/Icons/valid-xhtml-rdfa" alt="Valid XHTML + RDFa" /> </a> This content was extracted from <a 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