
Crevasse Valley Glacier
Glacier, Glaciology, Retreat of glaciers since 1850
Herausgegeben: Horst, Kristen Nehemiah
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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Crevasse Valley Glacier (76°46 S 145°30 WCoordinates: 76°46 S 145°30 W) 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.