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Miscast Nunataks : ウィキペディア英語版 | Miscast Nunataks The Miscast Nunataks () are a group of four nunataks which rise to on the south side of Byrd Glacier in Antarctica. The outcrops lie between Mount Tadpole and Mount Madison in the Churchill Mountains. The feature was geologically mapped as Dick Formation, a clastic, sandstone unit, by the New Zealand Geological Survey in 1960–61. The current name arose following remapping by United States Antarctic Program geologist Edmund Stump in 2000–01, and the determination that the entire outcrop is not sandstone but Shackleton Limestone.〔 ==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「Miscast Nunataks」の詳細全文を読む
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