Crevasse Valley Glacier

Crevasse Valley Glacier (76°46′S 145°30′W / 76.767°S 145.500°W / -76.767; -145.500Coordinates: 76°46′S 145°30′W / 76.767°S 145.500°W / -76.767; -145.500) is a broad glacier about 30 miles (50 km) long, flowing west-southwest between the Chester Mountains and the Saunders Mountain to the Sulzberger Ice Shelf in Marie Byrd Land, Antarctica. It was discovered by a sledging party of the Byrd Antarctic Expedition, which visited this area in November–December 1934, and so named because of its extensively crevassed surface.

See also

List of glaciers in the Antarctic

References

This article incorporates public domain material from the United States Geological Survey document "Crevasse Valley Glacier" (content from the Geographic Names Information System).

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