Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
公開日 |
1988-09-01 |
タイトル |
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タイトル |
RECONSTRUCTION OF MAXIMUM GLACIAL EXTENT IN THE CENTRAL SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
言語 |
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言語 |
eng |
資源タイプ |
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資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
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資源タイプ |
departmental bulletin paper |
ID登録 |
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ID登録 |
10.15094/00002569 |
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ID登録タイプ |
JaLC |
ページ属性 |
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内容記述タイプ |
Other |
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内容記述 |
P(論文) |
著者名よみ |
ヒラカワ, カズオミ
マツオカ, ノリカズ
モリワキ, キイチ
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著者名(英) |
HIRAKAWA, Kazuomi
MATSUOKA, Norikazu
MORIWAKI, Kiichi
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著者所属(英) |
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en |
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Department of Geography, Faculty of Education, Yamanashi University |
著者所属(英) |
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en |
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Institute of Geoscience, The University of Tsukuba |
著者所属(英) |
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en |
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National Institute of Polar Research |
抄録(英) |
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内容記述タイプ |
Other |
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内容記述 |
Glacial landforms and deposits indicating the past expansion of glaciers are described. It is conspicuous that thick erratics form an end-moraine ridge or an extensive depositional surface on the summit, and that roches moutonnees are developed on the sharp ridge. On the basis of these traces, a paleogeographical reconstruction during the time of the maximum glaciation is presented : (1) The southern half of the central Sør Rondane Mountains was mostly covered with the ice sheet from the ice plateau; (2) Ice fall was located 10km further north than at present; (3) Ice was about 300-350m thicker than at present; (4) The northern half of the central Sør Rondane Mountains rose relatively widely above the ice sheet and outlet glacier. |
雑誌書誌ID |
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収録物識別子タイプ |
NCID |
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収録物識別子 |
AA1072335X |
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences
巻 2,
p. 146-161,
発行日 1988-09
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出版者 |
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出版者 |
National Institute of Polar Research |