Crevasse Valley Glacier
| Crevasse Valley Glacier | |
|---|---|
  Location of Crevasse Valley Glacier in Antarctica | |
| Location | Marie Byrd Land |
| Coordinates | 76°46′S 145°30′W / 76.767°S 145.500°W |
| Length | 50 km (31 mi) |
| Thickness | unknown |
| Terminus | Sulzberger Bay |
| Status | unknown |
Crevasse Valley Glacier (76°46′S 145°30′W / 76.767°S 145.500°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, 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
References
This article incorporates public domain material from "Crevasse Valley Glacier". Geographic Names Information System. United States Geological Survey.
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