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Contortion Spur : ウィキペディア英語版 | Contortion Spur
Contortion Spur () is the largest and easternmost of three spurs which descend northwards from Mount Madison near the mouth of Byrd Glacier. The spur exposes a spectacular syncline of white marble and black schist. It was geologically mapped on December 10, 2000, by Edmund Stump of the United States Antarctic Program; he suggested the name because of the skewed form of the spur. ==References==
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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「Contortion Spur」の詳細全文を読む
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