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Bowman Glacier : ウィキペディア英語版 | Bowman Glacier
Bowman Glacier is a deeply entrenched glacier, long, descending the polar plateau between the Quarles Range and the Rawson Plateau of the Queen Maud Mountains to enter the Ross Ice Shelf just west of the flow of Amundsen Glacier. It was discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould, and named by Richard E. Byrd for Isaiah Bowman, an eminent geographer who was president of Johns Hopkins University, 1935–49, and Director of the American Geographical Society, 1915–35.〔 == 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「Bowman Glacier」の詳細全文を読む
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