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Epidote Peak : ウィキペディア英語版 | Epidote Peak Epidote Peak () is a prominent rock peak just north of the mouth of Held Glacier, overlooking the west side of Shackleton Glacier in the Queen Maud Mountains of Antarctica. It was so named by the Texas Tech Shackleton Glacier Expedition, 1964–65, because of the abundance of the mineral epidote which gives the peak a spotted appearance.〔 == 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「Epidote Peak」の詳細全文を読む
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