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Isocline Hill : ウィキペディア英語版 | Isocline Hill Isocline Hill () is a hill in the southern part of the Augen Bluffs, in the Miller Range, Antarctica. The hill rises above the west side of Marsh Glacier and is connected to the Augen Bluffs by a col lower than the height of the hill. It was so named by the Ohio State University Geological Party, 1967–68, because an isoclinal fold is well exposed on the side of the hill.〔 ==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「Isocline Hill」の詳細全文を読む
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