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LANDFORMS AROUND MT. RIISER-LARSEN, AMUNDSEN BAY, EAST ANTARCTICA
https://doi.org/10.15094/00002595
https://doi.org/10.15094/00002595391c6ba2-ad02-458c-8b61-62208b035152
名前 / ファイル | ライセンス | アクション |
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KJ00002368185 (62.8 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1989-09-01 | |||||
タイトル | ||||||
タイトル | LANDFORMS AROUND MT. RIISER-LARSEN, AMUNDSEN BAY, EAST ANTARCTICA | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00002595 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
記事種別(英) | ||||||
en | ||||||
ABSTRACT | ||||||
論文名よみ | ||||||
その他のタイトル | LANDFORMS AROUND MT. RIISER-LARSEN, AMUNDSEN BAY, EAST ANTARCTICA | |||||
著者名よみ |
アニヤ, マサム
× アニヤ, マサム× ハヤシ, マサヒサ |
|||||
著者名(英) |
ANIYA, Masamu
× ANIYA, Masamu× HAYASHI, Masahisa |
|||||
著者所属(英) | ||||||
en | ||||||
Institute of Geoscience, University of Tsukuba | ||||||
著者所属(英) | ||||||
en | ||||||
Faculty of Education, Shimane University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Landforms recognized in the Mt. Riiser-Larsen (about 1150m above the surrounding sea level) area, Amundsen Bay, Enderby Land, East Antarctica, were described and presented in a geomorphological map compiled from the result of field work and aerial photographic interpretation. Major landforms, primarily of glacial and periglacial origin, include aretes, cirques, free faces, slopes covered with frost-shattered rock fragments, talus and/or tills, moraines at several levels, glacio-fluvial channels and ponds, and sorted patterned grounds (mostly polygons).The till fields are located at several levels. From their locations, lithogical compositions, and the relative degree of development of patterned grounds on them, two levels were recognized to have been laid by the continental ice sheets (C-I and II), while four levels were judged to have been left by alpine glaciers (A-I, II, III and IV). Based on the distribution of these tills, the glacial sequence was inferred, although in a relative sense, as from older to newer, C-I, C-II, A-I, A-II, A-III, and A-IV. At present, it appears that the glaciation is not very active in this area, as three remaining small alpine glaciers appear to have been stagnant or started retreating. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1072335X | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences 巻 3, p. 142, 発行日 1989-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |