Crevasse Valley Glacier

Crevasse Valley Glacier (76°46′S 145°30′W) 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. 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).