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Statements

Subject Item
n36:_I–Z
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dbr:Stancomb-Wills_Glacier
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rdfs:label
斯坦科姆-威爾斯冰川 Stancomb-Wills-Gletscher Glaciar Stancomb-Wills Ghiacciaio Stancomb-Wills Stancomb-Wills Glacier Stancomb-Wills Glacier Stancomb-Willsgletsjer
rdfs:comment
Der Stancomb-Wills-Gletscher ist ein großer Gletscher an der Prinzessin-Martha-Küste des ostantarktischen Königin-Maud-Land. Er mündet südlich der Lyddan-Insel ins Weddell-Meer. Der Gletscher wurde am 5. November 1967 bei einem Flug der United States Navy entdeckt und vom United States Geological Survey anhand der dabei entstandenen Luftaufnahmen kartiert. Das Advisory Committee on Antarctic Names benannte ihn 1969 in Anlehnung an die Benennung nachfolgend beschriebener Gletscherzunge. The Stancomb-Wills Glacier is a large glacier that debouches into the eastern Weddell Sea southward of Lyddan Island. The glacier was discovered in the course of the U.S. Navy LC-130 plane flight over the coast on November 5, 1967, and was plotted by the United States Geological Survey (USGS) from photographs obtained at that time. The name was applied by the Advisory Committee on Antarctic Names (US-ACAN) in 1969. El glaciar Stancomb-Wills (del inglés: Stancomb-Wills Glacier) es un gran glaciar que vacía sus aguas en la parte oriental del mar de Weddell, al sur de la en la Antártida. El glaciar fue descubierto durante el trayecto sobre la costa del vuelo del aeroplano LC-130 de la Armada de Estados Unidos el 5 de noviembre de 1967, y fue cartografiado por la United States Geological Survey (USGS) a partir de fotografías obtenidas en el momento del descubrimiento. El nombre fue elegido por el Comité Consultivo sobre Nombres Antárticos (US-ACAN) en 1969. * Datos: Q1515008 De Stancomb-Willsgletsjer is een grote gletsjer aan de Prinses Marthakust van Koningin Maudland in Antarctica. De gletsjer eindigt ten zuiden van het eiland in de Weddellzee waar het de Stancomb-Willsgletsjertong vormt. De gletsjer werd ontdekt op 5 november 1967 tijdens een vlucht van de United States Navy en in kaart gebracht door het United States Geological Survey op basis van de gemaakte luchtfoto's. Het Advisory Committee on Antarctic Names gaf de gletsjer zijn naam in 1969 samen met de aanpassing van de benaming van de gletsjertong die hieronder wordt beschreven. Stancomb-Wills Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Norge gör anspråk på området. Stancomb-Wills Glacier ligger 28 meter över havet. Terrängen runt Stancomb-Wills Glacier är platt. Den högsta punkten i närheten är 292 meter över havet, 15,7 kilometer öster om Stancomb-Wills Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. 斯坦科姆-威爾斯冰川（英語：Stancomb-Wills Glacier）是南極洲的冰川，發源自毛德皇后地西部，最終在利丹島以南注入威德爾海東部，該冰川在1967年11月5日由美國海軍發現。 Il ghiacciaio Stancomb-Wills (in inglese "Stancomb-Wills glacier") è un ampio ghiacciaio situato sulla costa di Caird, nella Terra di Coats, in Antartide. Il ghiacciaio fluisce verso nord fino a terminare nel mare di Weddell, a sud dell' e costituisce quello che viene considerato il confine tra la Terra della Regina Maud e la Terra di Coats.
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Stancomb-Wills Glacier
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Location of Stancomb-Wills Glacier in Antarctica
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Penguin in Antarctica jumping out of the water.jpg
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Emperor penguins breed in the IBA
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dbo:abstract
Il ghiacciaio Stancomb-Wills (in inglese "Stancomb-Wills glacier") è un ampio ghiacciaio situato sulla costa di Caird, nella Terra di Coats, in Antartide. Il ghiacciaio fluisce verso nord fino a terminare nel mare di Weddell, a sud dell' e costituisce quello che viene considerato il confine tra la Terra della Regina Maud e la Terra di Coats. Der Stancomb-Wills-Gletscher ist ein großer Gletscher an der Prinzessin-Martha-Küste des ostantarktischen Königin-Maud-Land. Er mündet südlich der Lyddan-Insel ins Weddell-Meer. Der Gletscher wurde am 5. November 1967 bei einem Flug der United States Navy entdeckt und vom United States Geological Survey anhand der dabei entstandenen Luftaufnahmen kartiert. Das Advisory Committee on Antarctic Names benannte ihn 1969 in Anlehnung an die Benennung nachfolgend beschriebener Gletscherzunge. Die Stancomb-Wills-Gletscherzunge (75° 0′ S, 22° 0′ W) ist der ausgedehnte Fortsatz des Gletschers ins östliche Weddell-Meer. Sie wurde im Januar 1915 im Zuge der Endurance-Expedition (1914–1917) unter der Leitung des britischen Polarforschers Ernest Shackleton entdeckt. Shackleton hielt sie irrtümlich für ein Vorgebirge und benannte sie als Stancomb-Wills Promontory nach (1854–1932), eine der Hauptgeldgeberinnen der Expedition. 1970 passte das Advisory Committee on Antarctic Names die Benennung an die eigentliche Natur des Objekts an. The Stancomb-Wills Glacier is a large glacier that debouches into the eastern Weddell Sea southward of Lyddan Island. The glacier was discovered in the course of the U.S. Navy LC-130 plane flight over the coast on November 5, 1967, and was plotted by the United States Geological Survey (USGS) from photographs obtained at that time. The name was applied by the Advisory Committee on Antarctic Names (US-ACAN) in 1969. The Stancomb-Wills Glacier Tongue (75°0′S 22°0′W / 75.000°S 22.000°W) is the extensive seaward projection of the Stancomb-Wills Glacier into the eastern Weddell Sea. The cliffed front of this feature was discovered in January 1915 by a British expedition led by Shackleton. He named it "Stancomb-Wills Promontory," after Dame Janet Stancomb-Wills, one of the principal donors of the expedition. In 1969, US-ACAN amended the name to "Stancomb-Wills Glacier Tongue". This followed the U.S. Navy flight on which the glacier was discovered and the relationship with the glacier tongue was first observed. The Stancomb-Wills Glacier Important Bird Area (74°06′15″S 23°05′31″W / 74.10417°S 23.09194°W) is a 352 ha site which has been designated an Important Bird Area (IBA) by BirdLife International because it supports a breeding colony of about 5,500 emperor penguins, as estimated from 2009 satellite imagery, on fast ice on the north-eastern coast of the glacier tongue, some 60 km west of Lyddan Island. De Stancomb-Willsgletsjer is een grote gletsjer aan de Prinses Marthakust van Koningin Maudland in Antarctica. De gletsjer eindigt ten zuiden van het eiland in de Weddellzee waar het de Stancomb-Willsgletsjertong vormt. De gletsjer werd ontdekt op 5 november 1967 tijdens een vlucht van de United States Navy en in kaart gebracht door het United States Geological Survey op basis van de gemaakte luchtfoto's. Het Advisory Committee on Antarctic Names gaf de gletsjer zijn naam in 1969 samen met de aanpassing van de benaming van de gletsjertong die hieronder wordt beschreven. El glaciar Stancomb-Wills (del inglés: Stancomb-Wills Glacier) es un gran glaciar que vacía sus aguas en la parte oriental del mar de Weddell, al sur de la en la Antártida. El glaciar fue descubierto durante el trayecto sobre la costa del vuelo del aeroplano LC-130 de la Armada de Estados Unidos el 5 de noviembre de 1967, y fue cartografiado por la United States Geological Survey (USGS) a partir de fotografías obtenidas en el momento del descubrimiento. El nombre fue elegido por el Comité Consultivo sobre Nombres Antárticos (US-ACAN) en 1969. La lengua del glaciar (75°0′S 22°0′O / -75.000, -22.000), que se proyecta hacia el mar de Weddell, fue descubierta el 15 de enero de 1915 por una expedición británica dirigida por Ernest Shackleton, quien bautizó el sitio como "promontorio Stancomb-Wills" en honor de , una de las principales financiadoras de la expedición. En 1969, la US-ACAN enmendó el nombre como "lengua del glaciar Stancomb-Wills". * Datos: Q1515008 Stancomb-Wills Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Norge gör anspråk på området. Stancomb-Wills Glacier ligger 28 meter över havet. Terrängen runt Stancomb-Wills Glacier är platt. Den högsta punkten i närheten är 292 meter över havet, 15,7 kilometer öster om Stancomb-Wills Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten. 斯坦科姆-威爾斯冰川（英語：Stancomb-Wills Glacier）是南極洲的冰川，發源自毛德皇后地西部，最終在利丹島以南注入威德爾海東部，該冰川在1967年11月5日由美國海軍發現。
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