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Pegmatite Peak : ウィキペディア英語版 | Pegmatite Peak
Pegmatite Peak () is a peak (790 m) along the west side of Koerwitz Glacier, about midway between the main summits of Medina Peaks and Mount Salisbury, in the Queen Maud Mountains. First mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960-64. So named by New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1969–70, because of the occurrence of large, whitish pegmatite dykes in a rock wall at the southeast spur of the peak.
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「Pegmatite Peak」の詳細全文を読む
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