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Le glacier David est un glacier situé dans la terre Victoria, en Antarctique. Il avance dans la mer de Ross et forme la langue de glace Drygalski.
* Portail des lacs et cours d'eau
* Portail de la montagne
* Portail de l’Antarctique
, Der David-Gletscher ist der größte Gletsch … Der David-Gletscher ist der größte Gletscher des antarktischen Viktorialands. Vom nördlichen Polarplateau fließt er durch die Prince Albert Mountains und endet zwischen Kap Philippi und Kap Reynolds in Form der ins Rossmeer hineinragenden Drygalski-Eiszunge. Der Gletscher wurde von Teilnehmern der Nimrod-Expedition (1907–1909) unter der Leitung des britischen Polarforschers Ernest Shackleton entdeckt. Benannt ist er nach dem australischen Geologen Tannatt William Edgeworth David (1858–1934), der auf dieser Expedition unter anderem die Nordgruppe zur erfolgreichen Suche nach dem Ort des antarktischen magnetischen Pols leitete.s antarktischen magnetischen Pols leitete.
, Il ghiacciaio David è un ghiacciaio lungo … Il ghiacciaio David è un ghiacciaio lungo circa 110 km e largo circa 15 al termine, situato nella parte nord-occidentale della Dipendenza di Ross, nell'Antartide orientale. Il ghiacciaio, il cui punto più alto si trova a circa 1600 m s.l.m., si trova sulla costa di Scott, nella regione settentrionale delle montagne del Principe Alberto, dove fluisce verso est a partire da un nevaio di circa 200000 km², fino a entrare nel mare di Ross tra capo Philippi, a nord, e capo Reynolds, a sud.Lungo il suo percorso, il flusso del David è arricchito da quello dei ghiacciai Hollingsworth e Woodberry e, all'incirca a metà del percorso, dove incontra un forte dislivello nel terreno, esso si arricchisce di crepacci dando origine a quello che viene chiamato il "David Cauldron" (che in inglese significa letteralmente "calderone David"), infine, una volta giunto sulla costa, il ghiacciaio David forma sull'acqua la lingua glaciale Drygalski, lunga oltre 60 km.gua glaciale Drygalski, lunga oltre 60 km.
, David Glacier is the most imposing outlet … David Glacier is the most imposing outlet glacier in Victoria Land, Antarctica. It is named after the geologist Edgeworth David and is fed by two main flows which drain an area larger than 200,000 square kilometres of the East Antarctic plateau, with an estimated ice discharge rate of 7.8 +/- 0.7 km³/year. The northern flow drains from Talos Dome to the Ross Sea, but the main branch of the stream is fed by a network of tributaries which drain a common area of the inner plateau around Dome C and converge in a spectacular icefall normally known as the David Cauldron. The north wall of David Glacier, near its terminus at Cape Philippi, is named D'Urville Wall after Admiral Jules Dumont d'Urville. As the David Glacier flows into the Ross Sea, it forms a floating mass known as the Drygalski Ice Tongue. Hughes Bluff lies nearby.lski Ice Tongue. Hughes Bluff lies nearby.
, David Glacier är en glaciär i Antarktis. D … David Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Nya Zeeland och Australien gör anspråk på området. David Glacier ligger 1 046 meter över havet. Terrängen runt David Glacier är lite kuperad, och sluttar brant österut. Den högsta punkten i närheten är 1 405 meter över havet, 19,9 kilometer sydväst om David Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten.lkad. Det finns inga samhällen i närheten.
, 大衛冰川是南極洲的山峰，位於維多利亞地，流域面積20萬平方公里，最終注入羅斯海，冰體流量估計每年約7.8立方公里，附近有休斯海崖。
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David Glacier är en glaciär i Antarktis. D … David Glacier är en glaciär i Antarktis. Den ligger i Östantarktis. Nya Zeeland och Australien gör anspråk på området. David Glacier ligger 1 046 meter över havet. Terrängen runt David Glacier är lite kuperad, och sluttar brant österut. Den högsta punkten i närheten är 1 405 meter över havet, 19,9 kilometer sydväst om David Glacier. Trakten är obefolkad. Det finns inga samhällen i närheten.lkad. Det finns inga samhällen i närheten.
, Le glacier David est un glacier situé dans la terre Victoria, en Antarctique. Il avance dans la mer de Ross et forme la langue de glace Drygalski.
* Portail des lacs et cours d'eau
* Portail de la montagne
* Portail de l’Antarctique
, David Glacier is the most imposing outlet … David Glacier is the most imposing outlet glacier in Victoria Land, Antarctica. It is named after the geologist Edgeworth David and is fed by two main flows which drain an area larger than 200,000 square kilometres of the East Antarctic plateau, with an estimated ice discharge rate of 7.8 +/- 0.7 km³/year. The northern flow drains from Talos Dome to the Ross Sea, but the main branch of the stream is fed by a network of tributaries which drain a common area of the inner plateau around Dome C and converge in a spectacular icefall normally known as the David Cauldron. The north wall of David Glacier, near its terminus at Cape Philippi, is named D'Urville Wall after Admiral Jules Dumont d'Urville. As the David Glacier flows into the Ross Sea, it forms a floating mass known as the Drygalski Icea floating mass known as the Drygalski Ice
, Der David-Gletscher ist der größte Gletsch … Der David-Gletscher ist der größte Gletscher des antarktischen Viktorialands. Vom nördlichen Polarplateau fließt er durch die Prince Albert Mountains und endet zwischen Kap Philippi und Kap Reynolds in Form der ins Rossmeer hineinragenden Drygalski-Eiszunge.ossmeer hineinragenden Drygalski-Eiszunge.
, Il ghiacciaio David è un ghiacciaio lungo … Il ghiacciaio David è un ghiacciaio lungo circa 110 km e largo circa 15 al termine, situato nella parte nord-occidentale della Dipendenza di Ross, nell'Antartide orientale. Il ghiacciaio, il cui punto più alto si trova a circa 1600 m s.l.m., si trova sulla costa di Scott, nella regione settentrionale delle montagne del Principe Alberto, dove fluisce verso est a partire da un nevaio di circa 200000 km², fino a entrare nel mare di Ross tra capo Philippi, a nord, e capo Reynolds, a sud.Lungo il suo percorso, il flusso del David è arricchito da quello dei ghiacciai Hollingsworth e Woodberry e, all'incirca a metà del percorso, dove incontra un forte dislivello nel terreno, esso si arricchisce di crepacci dando origine a quello che viene chiamato il "David Cauldron" (che in inglese significa letid Cauldron" (che in inglese significa let
, 大衛冰川是南極洲的山峰，位於維多利亞地，流域面積20萬平方公里，最終注入羅斯海，冰體流量估計每年約7.8立方公里，附近有休斯海崖。
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David-Gletscher
, David Glacier
, Ghiacciaio David
, 大衛冰川
, Glacier David
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