Remington Glacier
78°34′00″S 84°18′00″W / 78.56667°S 84.30000°W / -78.56667; -84.30000
Remington Glacier is a steep glacier about 7 nautical miles (13 km; 8.1 mi) long in Doyran Heights in the Sentinel Range of Ellsworth Mountains, Antarctica. It rises just north of McPherson Peak and flows east-southeast to debouch between the terminus of Hough Glacier and Johnson Spur.
Background
![](http://upload.wikimedia.org/wikipedia/commons/thumb/6/6b/Vinson-Map.jpg/280px-Vinson-Map.jpg)
Discovered by U.S. Navy Squadron VX-6 on photographic flights of 14–15 December 1959, and mapped by United States Geological Survey (USGS) from these photos.[citation needed]
Named by Advisory Committee on Antarctic Names (US-ACAN) for Edward W. Remington, glaciologist at the South Pole Station during the IGY in 1957.[citation needed]
See also
- List of glaciers in the Antarctic
- Glaciology
Maps
- Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988.
- Antarctic Digital Database (ADD). Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly upgraded and updated.
References
- ^ Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988.
This article incorporates public domain material from "Remington Glacier". Geographic Names Information System. United States Geological Survey.
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- Outburst flood
- Overdeepening
- Periglaciation
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- Surge
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