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Dalgopol Glacier : ウィキペディア英語版 | Dalgopol Glacier
Dalgopol Glacier ((ブルガリア語:''ледник Дългопол''), ‘Lednik Galgopol’ \'led-nik d&l-go-'pol\) is a 3.4 km long glacier draining the northwest slopes of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated northeast of Vetrino Glacier and southwest of Kongur Glacier, and flows north of Mount Pisgah and northwest of Mezek Peak into Drake Passage. Bulgarian early mapping in 2009. The glacier is named after the town of Dalgopol in northeastern Bulgaria. ==Maps==
* L.L. Ivanov. (Antarctica: Livingston Island and Greenwich, Robert, Snow and Smith Islands. ) Scale 1:120000 topographic map. Troyan: Manfred Wörner Foundation, 2009. ISBN 978-954-92032-6-4
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「Dalgopol Glacier」の詳細全文を読む
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