Crevasse Valley Glacier
From Wikipedia, the free encyclopedia
Crevasse Valley Glacier () is a broad glacier about 30 miles (50 km) long, flowing west-southwest between Chester Mountains and Saunders Mountain to 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.
[edit] See also
This article incorporates text from Crevasse Valley Glacier, in the Geographic Names Information System, operated by the United States Geological Survey, and therefore a public domain work of the United States Government.
 |
This Antarctica or antarctic or sub-antarctic islands location article is a stub. You can help Wikipedia by expanding it. |
