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Pegmatite Point : ウィキペディア英語版 | Pegmatite Point
Pegmatite Point () is a distinctively banded point which juts into the head of Ross Ice Shelf from the Duncan Mountains. The point is 7 nautical miles (13 km) east-northeast of Mount Fairweather. It was first roughly plotted from ground surveys and aerial photographs by the Byrd Antarctic Expedition, 1928-30. The Southern Party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963–64, visited the point and gave the name because of the abundance of the rock Pegmatite.
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 Point」の詳細全文を読む
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