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アイテム
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越後平野の「0m地帯」と浸水被害予測
http://hdl.handle.net/10191/39275
http://hdl.handle.net/10191/392755473e05c-6cae-4b03-a62f-65f68bd47616
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2016-03-08 | |||||
タイトル | ||||||
タイトル | 越後平野の「0m地帯」と浸水被害予測 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 越後平野の「0m地帯」と浸水被害予測 | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Echigo Plain | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Lowland below the sea level | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | subsidence of ground | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | inland earthquake | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 越後平野 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 0m地帯 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 地盤の沈降 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 直下型地震 | |||||
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 | Distribution of the lowland below the mean sea level zero meter area and prediction of the inundated damage in the Echigo Plain. | |||||
著者 |
高濱, 信行
× 高濱, 信行× ト部, 厚志 |
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著者別名 | ||||||
識別子 | 160558 | |||||
識別子Scheme | WEKO | |||||
姓名 | Takahama, Nobuyuki | |||||
著者別名 | ||||||
識別子 | 160559 | |||||
識別子Scheme | WEKO | |||||
姓名 | Urabe, Atsushi | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Echigo Plain facing the Sea of Japan is formed the coastal plain with area of 2,070 km^2. Many rivers such as Shinano River and Agano River flow into this coastal plain, and formed the wide lowland. In the Niigata City with the river mouth of the two rivers, the lowland below the mean sea level “zero meter area” is widely extends. In this area, the occurrence of the widely inundated damage is predicted that the levee breach by flooding or earthquake, tsunami and storm surge are happened. Recently, the formative history of the Echigo Plain is reexamined from the investigation of remains and borehole data. These results show the high possibility that the swamp or pond will be formed by the subsidence of the ground involved the inland earthquake. The subsidence by the inland earthquake has presented the new problem, which is not included for the estimation of the earthquake damage of the Niigata region. | |||||
書誌情報 |
新潟大学積雪地域災害研究センター研究年報 en : 新潟大学積雪地域災害研究センター研究年報 巻 27, p. 11-18, 発行日 2005-12 |
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出版者 | ||||||
出版者 | 新潟大学積雪地域災害研究センター | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 03877892 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00183327 | |||||
著者版フラグ | ||||||
値 | publisher |