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Crevasse Valley Glacier : ウィキペディア英語版 | Crevasse Valley Glacier Crevasse Valley Glacier () is a broad glacier about 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==
* List of glaciers in the Antarctic
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Crevasse Valley Glacier」の詳細全文を読む
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