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GEOMORPHOLOGY OF KASUMI ROCK ON THE PRINCE OLAV COAST, EAST ANTARCTICA
https://doi.org/10.15094/00002772
https://doi.org/10.15094/0000277261ce024a-03f7-4aa7-8a8e-6dec96eca77b
名前 / ファイル | ライセンス | アクション |
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KJ00002368402 (55.5 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1994-09-01 | |||||
タイトル | ||||||
タイトル | GEOMORPHOLOGY OF KASUMI ROCK ON THE PRINCE OLAV COAST, 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 | 10.15094/00002772 | |||||
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 | GEOMORPHOLOGY OF KASUMI ROCK ON THE PRINCE OLAV COAST, EAST ANTARCTICA | |||||
著者名よみ |
ハヤシ, マサヒサ
× ハヤシ, マサヒサ |
|||||
著者名(英) |
HAYASHI, Masahisa
× HAYASHI, Masahisa |
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著者所属(英) | ||||||
en | ||||||
Department of Geography, Faculty of Education, Shimane University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Kasumi Rock is a small and hilly ice-free area below 50m asl formed by ice sheet erosion. The freshness of this glaciated feature suggests the retreat of ice sheet occurred during considerably later period than the other areas of the Coast. Glacial striation shows the direction N35-45°W. The following topographic features are observed from the southern ice margin toward the northern sea : (1) Ice sheet margin with shear planes dipping 5°S. (2) Narrow till field where patterned ground, especially polygons as large as 5m in diameter, are well developed. (3) Undulating bedrock surface 35 to 45m high where stoss-and-lee topography is covered with scattered erratics. (4) Undulating bedrock surface 25 to 35m high. Stoss-and-lee topography also develops but erratics are rarely found. (5) Hilly topography with jagged bedrock surface excavated by weathering such as tafoni. (6) Steep break stretching in the W-E direction 20m in relative height, (7) Smoothed flat bedrock surface like a strandflat lower than 10m asl with patches of beach deposits. Marine sand is recognized up to 6m asl. Several ridges of lateral moraine rising about 5m in relative height demarcate the western margin of this area. They show that the lateral margin of Itime Glacier, an outlet glacier, retreated westward by 50 to 100m during recent time. | |||||
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 7, p. 190, 発行日 1994-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |