Bowman Glacier

Bowman Glacier is a deeply entrenched glacier, 40 nautical miles (70 km) long, descending the polar plateau between the Quarles Range and the Rawson Plateau of the Queen Maud Mountains to enter the Ross Ice Shelf just west of the flow of Amundsen Glacier. It was discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould, and named by Richard E. Byrd for Isaiah Bowman, an eminent geographer who was president of Johns Hopkins University, 1935–49, and Director of the American Geographical Society, 1915–35.[1]

Bowman Glacier
Map showing the location of Bowman Glacier
Map showing the location of Bowman Glacier
Location of Bowman Glacier in Antarctica
LocationRoss Dependency
Coordinates85°34′S 162°00′W
Length40 nmi (74 km; 46 mi)
Thicknessunknown
TerminusRoss Ice Shelf
Statusunknown

See also

References
  1. "Bowman Glacier". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2011-08-10.

Public Domain This article incorporates public domain material from "Bowman Glacier". Geographic Names Information System. United States Geological Survey.


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