Denman Glacier
Denman Glacier is a glacier 7 to 10 miles (11 to 16 km) wide, descending north some 70 miles (110 km), which debouches into the Shackleton Ice Shelf east of David Island, Queen Mary Land. It was discovered in November 1912 by the Western Base party of the Australasian Antarctic Expedition under Sir Douglas Mawson. Mawson named the glacier for Lord Denman, Governor-General of Australia in 1911, a patron of the expedition. Calving of Denman Glacier into the Mawson Sea gives rise to the periodically appearing Pobeda Ice Island.
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Denman Glacier
Denman Glacier is a glacier 7 to 10 miles (11 to 16 km) wide, descending north some 70 miles (110 km), which debouches into the Shackleton Ice Shelf east of David Island, Queen Mary Land. It was discovered in November 1912 by the Western Base party of the Australasian Antarctic Expedition under Sir Douglas Mawson. Mawson named the glacier for Lord Denman, Governor-General of Australia in 1911, a patron of the expedition. Calving of Denman Glacier into the Mawson Sea gives rise to the periodically appearing Pobeda Ice Island.
has abstract
Denman Glacier is a glacier 7 ...... y appearing Pobeda Ice Island.
@en
Der Denman-Gletscher ist ein G ...... chirmherr der Forschungsreise.
@de
登曼冰川是南極洲的冰川,全長約110公里,寬11至16公里, ...... 个與南极洲地理相關的小作品。你可以通过编辑或修订扩充其内容。
@zh
Wikipage page ID
Wikipage revision ID
691,752,363
hypernym
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-66.75 99.5
comment
Denman Glacier is a glacier 7 ...... y appearing Pobeda Ice Island.
@en
Der Denman-Gletscher ist ein G ...... chirmherr der Forschungsreise.
@de
登曼冰川是南極洲的冰川,全長約110公里,寬11至16公里, ...... 个與南极洲地理相關的小作品。你可以通过编辑或修订扩充其内容。
@zh
label
Denman Glacier
@en
Denman-Gletscher
@de
登曼冰川
@zh