北海道登別市における1980年8月豪雨による斜面崩壊

書誌事項

タイトル別名
  • Slope-Failure Caused by Heavy Rain Fall of August, 1980, Noboribetsu City, Hokkaido, Japan
  • ホッカイドウ ノボリベツシ ニ オケル 1980ネン 8ガツ ゴウウ ニヨル

この論文をさがす

説明

In August, 1980, a great number of slope-failure occurred at Tomiura area, Noboribetsu City. In this area, late Pleistocene pyroclastic deposits of Kuttara Volcano are widely developed.<BR>Results obtained from this study are as follows:<BR>1. The slope-failure is caused by heavy rains with maximum intensity reaching 40-60 mm/hour.<BR>2. The original slope-failure is produced by the abundance of water absorbed by the piping system of the slope, is occurred at the cutting slope of the City Road and Route 36.<BR>3. At the top of the natural slope, hollowed area, secondary collapse and gully erosion occurred, producing the debris flow. This debris flow ran down the valley wall taking off the surface soils and made the gullies.

収録刊行物

  • 応用地質

    応用地質 23 (4), 221-229, 1982

    一般社団法人 日本応用地質学会

キーワード

詳細情報 詳細情報について

問題の指摘

ページトップへ