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Grand Chasms : ウィキペディア英語版 | Grand Chasms
The Crand Chasms () are two or more deep crevasses in the Filchner Ice Shelf, Antarctica, extending west for an unknown distance from 37°W, close west of the Touchdown Hills. The feature is the most notable crevassed area on the Filchner Ice Shelf, roughly long and from wide. It was discovered by the Commonwealth Trans-Antarctic Expedition, 1955-58. During 1957 it was examined by a U.S. party from Ellsworth Station led by Dr. Edward Thiel, who applied the descriptive name.〔 ==References==
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「Grand Chasms」の詳細全文を読む
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