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Mount Drewry (84°27′S 167°21′E) is a prominent blocklike mountain on the west side of Beardmore Glacier, rising to 2,910 metres (9,550 ft) between Bingley Glacier and Cherry Icefall in the Queen Alexandra Range. It was discovered and roughly mapped by the Southern Journey Party of the British Antarctic Expedition, 1907–09, led by Ernest Shackleton, which was abreast of this mountain on 13 December 1908. It was named by the Advisory Committee on Antarctic Names in 1986 after David J. Drewry, a British glaciologist who was a leader of the Scott Polar Research Institute – National Science Foundation – Technical University of Denmark airborne radio echo sounding program, 1967–79, Director of the Scott Polar Research Institute, 1984–87, and Director of the British Antarctic Survey, from 1987.[1]


References


  1. "Drewry, Mount". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 31 January 2012.

 This article incorporates public domain material from the United States Geological Survey document: "Drewry, Mount". (content from the Geographic Names Information System)



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[de] Mount Drewry

Mount Drewry ist ein 2910 m hoher und markanter Berg in der antarktischen Ross Dependency. In der Königin-Alexandra-Kette des Transantarktischen Gebirges ragt er zwischen dem Bingley-Gletscher und dem Cherry-Eisfall an der Westflanke des Beardmore-Gletschers auf.
- [en] Mount Drewry



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