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北海道，網走・北見・津別地域の地すべり（第２報） -美幌地域での地すべり地形の特徴と最近の地すべり-
https://kitami-it.repo.nii.ac.jp/records/6705
https://kitami-it.repo.nii.ac.jp/records/67051197d8c2-8815-4418-8252-3435b736c5bf
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
25-1-10.pdf (4.3 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，網走・北見・津別地域の地すべり（第２報） -美幌地域での地すべり地形の特徴と最近の地すべり- | |||||
| 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 | Landslides in the Abashiri-Kitami-Tsubetsu district，Hokkaido，Japan(part 2)；Characteristics of landslide configurations an recent landslides in the Bihoro district | |||||
| 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 | 33827 | |||||
| 姓名 | Yoji, ITO | |||||
| 言語 | en | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | In the topographic map "Bihoro"1 : 50，000 in scale situated in the central part of the Abashiri-Kitami-Tsubetsu landslide concentration region, 168 landslide configurations were recognized in aeria-photographs. Most of them are concentrated in the western area，which consists of siltstone and hard shale with interbeds of thin layers of tuff, the so-called Miocene Tsubetsu Formation. This is presumably related to the siltstone and shale which disintegrated into small fragments to mud by weathering and to the clayey tuff beds. Most of the landslide configurations show morphology of small scale debris slump (A type) and debris slide (C and F types) in this area. The directions of landslide debris movement are mostly ENE to ESE. Moreover，landslide configurations are found sporadically along the boundary between Quaternary welded tuffs or the Bihoro Formation which is composed of gravel and sand, and overlying pumice flow deposits in the eastern area. In this area， most of them are small-scale debris slide (F type). Since some recent landslide disasters were caused by the re-sliding of older landslide debris，it is necessary to care of landslide configurations at the planning and investigating stages of developments. | |||||
| 言語 | en | |||||
| 書誌情報 |
ja : 北見工業大学研究報告 巻 25, 号 1, p. 95-106, 発行日 1993-09 |
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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 | |||||
