Crevasse Valley Glacier
|Crevasse Valley Glacier|
|Location||Marie Byrd Land|
|Length||50 km (31 mi)|
Crevasse Valley Glacier (Coordinates: ) 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.
- This article incorporates public domain material from the United States Geological Survey document "Crevasse Valley Glacier" (content from the Geographic Names Information System).
|This Marie Byrd Land location article is a stub. You can help Wikipedia by expanding it.|
|This glaciology article is a stub. You can help Wikipedia by expanding it.|