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Geomorphological mapping in the adjacent area to Syowa Station (abstract)
https://nipr.repo.nii.ac.jp/records/1486
https://nipr.repo.nii.ac.jp/records/14865dad83c5-189a-451c-a1d2-94e6267aae14
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000012119 (62.5 kB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1983-10-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Geomorphological mapping in the adjacent area to Syowa Station (abstract) | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Hirakawa, Kazuomi
× Hirakawa, Kazuomi× Ono, Yugo |
|||||
著者所属(英) | ||||||
en | ||||||
Yamanashi University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Science, The University of Tsukuba | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Detailed geomorphological mapping in Antarctica is in progress as examplified by the sheet Langhovde 1 : 25,000,near Syowa Station. The information on the geomorphological map is divided into several groups; 1) topography (including contour lines), 2) morphometry and/or morphography, 3) subsurface materials and/or basement rocks and 4) geomorphic processes. Each morphography, such as cliffs, valley forms, breaks and steps of slopes and so on, is mapped, on the basis of the airphoto interpretation. It is most important to decide the areas presented by colors. In this case, they are 1) area of geomorphic processes such as periglacial, fluvioglacial or glacial ones and 2) area of several types of basement rocks which strongly control the relief of the studied region. Some morphographies closely related to the certain processes could be also given by the individual colors. Active geomorphic processes are indicated by the special symbols. This geomorphological map is prepared with special reference to the methods in France and the Federal Republic of Germany. The geomorphological mapping will be continued in the other regions of Antarctica, especially in the inland mountainous region, because such map is necessary as the basic data for understanding the geomorphic development and geomorphic processes in Antarctica. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 28, p. 259, 発行日 1983-10 |