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Harrisson Ice Rises : ウィキペディア英語版 | Harrisson Ice Rises The Harrisson Ice Rises () are a local swelling of the ice surface west-southwest of Henderson Island, Antarctica, where the Shackleton Ice Shelf overrides an underlying obstruction. The feature was discovered by the Eastern Sledge Party of the Australasian Antarctic Expedition (1911–14) under Douglas Mawson, who named the feature for Charles T. Harrisson, biologist with the expedition.〔 ==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「Harrisson Ice Rises」の詳細全文を読む
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