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アイテム
北海道東部，知床半島における大規模地すべり・崩壊地形の特徴
https://kitami-it.repo.nii.ac.jp/records/6720
https://kitami-it.repo.nii.ac.jp/records/6720ad85bcc2-8cda-453a-9ca6-8c075fe77492
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
26-1-3.pdf (6.7 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2007-04-09 | |||||
| タイトル | ||||||
| タイトル | 北海道東部，知床半島における大規模地すべり・崩壊地形の特徴 | |||||
| 言語 | ja | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| 資源タイプ | ||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||
| タイプ | departmental bulletin paper | |||||
| その他のタイトル | ||||||
| その他のタイトル | Characteristics of large-scale landslides in the Shiretoko Peninsula, Eastern Hokkaido, Japan. | |||||
| 言語 | en | |||||
| 著者 |
伊藤, 陽司
× 伊藤, 陽司 |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 33885 | |||||
| 姓名 | Yoji, ITO | |||||
| 言語 | en | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The Shiretoko Peninsula in eastern Hokkaido is known for its abundance of landslides. In this region，a total of 606 landslides were identified in aerial photographs of which 97 were large-scale landslides (more than 500 m wide or 20 ha in area). The characteristics of large-scale landslides in the Shiretoko Peninsula are summarized as follows : 1)Large-scale landslides are mostly found along the margins of Pliocene to Quaternary subaerial andesitic lavas overlying Miocene volcaniclastic and clastic rocks. One of the geological factors for large-scale landslides is cap rock structures composed of subaerial lavas and underlying Miocene strata， which are susceptible to small-scale landsliding. 2)Most large-scale landslides are of rock-slump-type shape or debris-avalanche-type shape，the latter of which is characterized by a main scarp with large relative elevation, sliding mass under the scarp, and sliding/flowing debris of several hundreds meters in length. Moreover，also recognized were debris flows forming the waste-filled valleys of 400 to 500 meters wide and 3 to 4 kilometers long. 3) Moving and depositional areas in large-scale landslides were mostly enlarged by the repeated occurrence of landslides and flows of sliding mass， and the new sliding occured on the back-slope of the main scarp. 4)In order to understand the mechanism of large-scale sliding， the relationships of the Rausudake active faults and the destruction of the dome-like volcaro to the Onnebetsudake large-scale landslides should be further investigated in detail. | |||||
| 言語 | en | |||||
| 書誌情報 |
ja : 北見工業大学研究報告 巻 26, 号 1, p. 15-28, 発行日 1994-09 |
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| フォーマット | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | application/pdf | |||||
| 著者版フラグ | ||||||
| 言語 | en | |||||
| 値 | publisher | |||||
| 出版者 | ||||||
| 出版者 | 北見工業大学 | |||||
| 言語 | ja | |||||
