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東オングル島水汲み沢の隆起汀線の地形と周氷河地形(日本南極地域観測隊の報告)
https://doi.org/10.15094/00007701
https://doi.org/10.15094/00007701c4f85b12-bb05-406f-b3a6-e4390d7af1b0
名前 / ファイル | ライセンス | アクション |
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KJ00002476701 (11.5 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1973-03-01 | |||||
タイトル | ||||||
タイトル | 東オングル島水汲み沢の隆起汀線の地形と周氷河地形(日本南極地域観測隊の報告) | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | The Landforms of the Mizukumi Zawa near Syowa Station, East Antarctica (Reports of the Japanese Antarctic Research Expedition) | |||||
言語 | ||||||
言語 | jpn | |||||
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 | 10.15094/00007701 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | ヒガシ オングル トウ ミズクミザワ ノ リュウキ テイセン ノ チケイ ト シュウヒョウガ チケイ ニホン ナンキョク カンソクタイ ノ ホウコク | |||||
著者名(日) |
藤原, 健蔵
× 藤原, 健蔵 |
|||||
著者名(英) |
FUJIWARA, Kenzo
× FUJIWARA, Kenzo |
|||||
著者所属(日) | ||||||
広島大学教養部地理学教室 | ||||||
著者所属(英) | ||||||
en | ||||||
College of General Education, Hiroshima University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Based on the investigation of micro-reliefs and deposits of the Mizukumi Zawa (Valley), which is a small glacial trough near Syowa Station, geomorphic evolution after recession of ice sheet was studied. The valley floor in the investigated area was divided into five raised beaches and gentle slopes above them. The raised beaches are referred to as surfaces I (14.0-11.5m. a. s. l.), II (10.0-9.5m.), III (7.0-6.0m.), IV (4.5-3.0m.) and V (below 2.0m.), surface I being the oldest. The molluscan shells contained in the deposits of surfaces I gave a ^<14>C date a little older than 30,000yr. B. P. and the surface V date 3,000-6,000yr. B. P. (YOSHIDA, 1970). Therefore, it seems that surfaces I and V were formed owing to the marine transgressions during the interstadial oscillation that preceded the Late Wurm glaciation and during the postglacial age, respectively. Surface II is a product of the marine regression that followed immediately after the interstadial oscillation. It is impossible to date definitely surfaces III and IV, which are composed of thick coarse materials, because the radiocarbon ages of shells on the surfaces range widely from 20,000 to 31,000yr. B. P. As a rule periglacial processes in this area are slight, on account of the summer weather with relatively few freeze-thaw cycles and low precipitation. The gentle slopes, constituting the upper part of valley floor, are the result of the repeated freeze-thaw which shatters the bedrock and of the solifluction which removes the debris. The upper slope at the foot of valley walls is the steepest, and is the source of the slope debris. The middle and lower slopes have smooth surfaces with low angles and are covered with fine debris of freeze-thaw. And, the north-facing slopes are developed better than the south-facing ones. The processes that account for such characters of these gentle slopes are discussed. Other landforms, such as cryoturbation steps, patterned ground and rock shattering, are also described. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00181831 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00857289 | |||||
書誌情報 |
南極資料 巻 46, p. 44-66, 発行日 1973-03 |
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国際十進分類法 | ||||||
主題Scheme | UDC | |||||
主題 | 551.4:551.77/.79 | |||||
出版者 | ||||||
出版者 | 国立極地研究所 |