Denman Glacier
Denman Glacier | |
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Location of Denman Glacier in Antarctica | |
Type | tributary |
Location | Queen Mary Land |
Coordinates | 66°45′S 99°30′E / 66.750°S 99.500°E / -66.750; 99.500 |
Length | 70 nmi (130 km; 80 mi) |
Width | 10 nmi (19 km; 12 mi) |
Thickness | unknown |
Terminus | Shackleton Ice Shelf |
Status | unknown |
Denman Glacier is a glacier 7 to 10 nautical miles (13 to 19 km; 8 to 12 mi) wide, descending north some 70 nautical miles (130 km; 80 mi), 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.[1]
Calving of Denman Glacier into the Mawson Sea gives rise to the periodically appearing Pobeda Ice Island.
See also
References
- ↑ "Denman Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2012-01-11.
Coordinates: 66°45′S 99°30′E / 66.750°S 99.500°E / -66.750; 99.500
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Glaciers of Queen Mary Land | |
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