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Mill Glacier : ウィキペディア英語版 | Mill Glacier
Mill Glacier is a tributary glacier, wide, flowing northwest between the Dominion Range and the Supporters Range into Beardmore Glacier, Antarctica. It was discovered by the British Antarctic Expedition, 1907–09, and named for Hugh Robert Mill, a British geographer and Antarctic historian.〔 ==See also==
* List of glaciers in the Antarctic
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「Mill Glacier」の詳細全文を読む
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