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2004年新潟県中越地域2大同時多発斜面災害の特徴と比較
http://hdl.handle.net/10191/1189
http://hdl.handle.net/10191/118955fdb400-d8f4-42cf-a446-10f66af1411c
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
25_0020.pdf (4.3 MB)
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| Item type | テクニカルレポート / Technical Report(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2007-04-23 | |||||
| タイトル | ||||||
| タイトル | 2004年新潟県中越地域2大同時多発斜面災害の特徴と比較 | |||||
| タイトル | ||||||
| タイトル | 2004年新潟県中越地域2大同時多発斜面災害の特徴と比較 | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | 地すべり | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | 崩壊 | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | 7.13豪雨 | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | 10.23中越地震 | |||||
| 資源タイプ | ||||||
| 資源 | http://purl.org/coar/resource_type/c_18gh | |||||
| タイプ | technical report | |||||
| その他のタイトル | ||||||
| その他のタイトル | Characteristics and comparison between many simultaneous landslides in Chuetsu region, Niigata, Japan, in 2004 | |||||
| 著者 |
山岸, 宏光
× 山岸, 宏光× 丸井, 英明× 渡部, 直樹× 川邊, 洋× Ayalew, Lulseged |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 175660 | |||||
| 姓名 | Yamagishi, Hiromitsu | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 175661 | |||||
| 姓名 | Marui, Hideaki | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 175662 | |||||
| 姓名 | Watanabe, Naoki | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 175663 | |||||
| 姓名 | Kawanabe, Hiroshi | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | On July 13, 2004, heavy rainfalls due to the intensive activities of rain front occurred in the Mid Niigata Region, Japan. They are as much as 400mm in 24 hours, bringing about serious flooding by breaking the river banks. The heavy rainfalls also triggered more than 3600 landslides. The floods and landslides in total claimed 15 lives, all of whom were characteristically old persons. Three months later of such hydrological disasters, the southern region of Mid Niigata Region was attacked by intensive earthquake of M.6.8 on Richter Scale on October 23, 2004. The main earthquake were followed by intensive after shocks which continued until December 2004. By these earthquakes, many landslides also occurred in the hilly and mountainous areas. Namely, different triggers for the landslides have been experienced in the similar geological and geomorphological region. Hence, we have classified the by 7.13 rainfall landslides into two types; surface failures and deep-seated slides with long-run mudflows. While, we have divided the 10.23 earthquake landslides into three types; surface failures, flow type slides and deep-seated slides. | |||||
| 書誌情報 |
新潟県連続災害の検証と復興への視点 en : 新潟県連続災害の検証と復興への視点 p. 140-147, 発行日 2005-08 |
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| 出版者 | ||||||
| 出版者 | 災害復興科学センター | |||||
| 書誌レコードID | ||||||
| 識別子タイプ | NCID | |||||
| 関連識別子 | BA73361841 | |||||
| 著者版フラグ | ||||||
| 値 | publisher | |||||
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Cite as
山岸, 宏光, 丸井, 英明, 渡部, 直樹, 川邊, 洋, Ayalew, Lulseged, 2005, 2004年新潟県中越地域2大同時多発斜面災害の特徴と比較: 災害復興科学センター, 140–147 p.
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