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  1. 0 資料タイプ別
  2. 03 紀要論文
  1. 360 災害・復興科学研究所
  2. 20 紀要
  3. 90 新潟大学積雪地域災害研究センター研究年報
  4. 第1号

1978年5月18日妙高災害(1) : 斜面崩壊について

http://hdl.handle.net/10191/38976
http://hdl.handle.net/10191/38976
4a0afb8d-ca79-4abf-a533-0d2d09c6747e
名前 / ファイル ライセンス アクション
1_1-21.pdf 1_1-21.pdf (1.8 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2016-03-03
タイトル
タイトル 1978年5月18日妙高災害(1) : 斜面崩壊について
タイトル
言語 en
タイトル 1978年5月18日妙高災害(1) : 斜面崩壊について
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 Cause of landslide occurred at Mt. Myoko on 18th May, 1978
著者 青木, 滋

× 青木, 滋

WEKO 162175

青木, 滋

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藤田, 至則

× 藤田, 至則

WEKO 162176

藤田, 至則

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霜鳥, 重雄

× 霜鳥, 重雄

WEKO 162177

霜鳥, 重雄

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島津, 光夫

× 島津, 光夫

WEKO 162178

島津, 光夫

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吉村, 尚久

× 吉村, 尚久

WEKO 162179

吉村, 尚久

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高浜, 信行

× 高浜, 信行

WEKO 162180

高浜, 信行

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早川, 嘉一

× 早川, 嘉一

WEKO 162181

早川, 嘉一

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北野, 康

× 北野, 康

WEKO 162182

北野, 康

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鈴木, 幸治

× 鈴木, 幸治

WEKO 162183

鈴木, 幸治

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著者別名
識別子 162184
識別子Scheme WEKO
姓名 Aoki, Shigeru
著者別名
識別子 162185
識別子Scheme WEKO
姓名 Fujita, Yukinori
著者別名
識別子 162186
識別子Scheme WEKO
姓名 Shimotori, Shigeo
著者別名
識別子 162187
識別子Scheme WEKO
姓名 Shimazu, Mitsuo
著者別名
識別子 162188
識別子Scheme WEKO
姓名 Yoshimura, Takahisa
著者別名
識別子 162189
識別子Scheme WEKO
姓名 Takahama, Nobuyuki
著者別名
識別子 162190
識別子Scheme WEKO
姓名 Hayakawa, Kaichi
著者別名
識別子 162191
識別子Scheme WEKO
姓名 Kitano, Yasushi
著者別名
識別子 162192
識別子Scheme WEKO
姓名 Suzuki, Koji
抄録
内容記述タイプ Abstract
内容記述 1) At about 6:20 a.m. on 18th May, 1978, the slope area of 1.3ha, located at 1,600 m above the sea level, was suddenly broken and a mass of about 200,000 m^3 were sliden into the valley of river Shirotagiri-gawa (Loc. 1 in Fig. 1). 2) The broken slope consisted mainly of surface materials which can be subdivided into permeable and channel which are composed of altered andesitic tuff breccia, as shown in Figs.11, 19 and 20. 3) The groundwater of landslide site can be subdivided into two types; one is shallow water in buried river deposits (A_2-type) and another is fissure water involved in altered bed rock (A_1-type) as shown in Figs.8 and 20. The tritium content in both types of water is nearly the same as that of recent rain water. 4) The surface materials seem to have been moved sometimes in the past, and as a result of such occasional movement, the crack which coincides with slide surface would be originated in the talus deposits, as shown in Fig.1 of plate III and in Fig.17. 5) It is strongly suggested that the infiltration of large amount of water, which was supplied from rapid snow melting at unusual high temperature in that season, might increased the pore water pressure in the surface deposits to break the above-mentioned unstable state of slope, and the landslide was brought about in succession.
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 1, p. 1-21, 発行日 1979-03
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
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