The David Glacier (75°19′S162°00′E / 75.317°S 162.000°E / -75.317; 162.000) is a glacier over 60 nautical miles (110 km; 69 mi) long, flowing east from the polar plateau through the Prince Albert Mountains to the coast of Victoria Land, Antarctica. It enters Ross Sea between Cape Philippi and Cape Reynolds to form the floating Drygalski Ice Tongue.[1]
It is the most imposing outlet glacier in Victoria Land. It is fed by two main flows which drain an area larger than 200,000 square kilometres, with an estimated ice discharge rate of 7.8 +/- 0.7 km3/year.[2]
The David Glacier was discovered by Ernest Shackleton's "Northern Party," in November 1908, under the leadership of Prof. T.W. Edgeworth David, of Sydney University, for whom the feature was named.[1]
The DavidGlacier (75°19′S 162°00′E / 75.317°S 162.000°E / -75.317; 162.000) is a glacier over 60 nautical miles (110 km; 69 mi) long, flowing east...
A glacier (US: /ˈɡleɪʃər/; UK: /ˈɡlæsiər, ˈɡleɪsiər/) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms...
German explorer then in Antarctica. The glacier that feeds the ice tongue was named after Edgeworth David. David and Douglas Mawson crossed the ice tongue...
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(south) by Emmanuel Glacier, Zoller Glacier, Darkowski Glacier, Bol Glacier, Condit Glacier, Descent Glacier and Overflow Glacier. From the right it is...
line at its mouth. It has the largest catchment area between DavidGlacier and Byrd Glacier, and drains about 5.23±0.59 gigatonnes of ice per year into...
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Glacier is a glacier 11 to 16 km (7 to 10 mi) wide, descending north some 110 km (70 mi), which debouches into the Shackleton Ice Shelf east of David...