Wright Upper Glacier
Wright Upper Glacier (77°32′S 160°35′E / 77.533°S 160.583°E) is an ice apron at the upper west end of Wright Valley in Asgard Range, Antarctica. It is formed by a glacier flowing east from the inland ice plateau. Named by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59) for C.S. Wright, a member of the British Antarctic Expedition (1910–13), after whom the "Wright Glacier" (adjusted to Wright Lower Glacier by the VUWAE) was named.[1]
Two massive icefalls descend from the plateau into the Wright Upper Glacier, the 5 km (3.1 mi) wide and 400 m (1,300 ft) tall Airdevronsix Icefalls and the equally tall 0.92 km (0.57 mi) wide Warren Icefalls, which was named by the Advisory Committee on Antarctic Names (US-ACAN) in 2004 for Alden Warren, a longtime photographer (scientific and technical) with the United States Geological Survey, involved in documenting maps of Antarctica.[2][3]
Vortex Col is a col leading from the plateau into the south side of the glacier. At this locality, winds carrying clouds of snow from the polar plateau are deflected by Mount Fleming and funneled down this depression. The descriptive name was given by New Zealand Antarctic Place-Names Committee (NZ-APC).[4]
References
- ^ "Wright Upper Glacier". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2018-09-03.
- ^ "Warren Icefall". Wondermondo. 2014-07-07. Retrieved 2019-06-10.
- ^ "Warren Icefall". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2018-09-03.
- ^ "Vortex Col". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2018-09-03.
This article incorporates public domain material from websites or documents of the United States Geological Survey.
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