地すべり運動の地質学的解明

• 山野井 徹

  山形大学理学部地球環境学科

書誌事項

タイトル別名

• Geologic clarifications of a landslide movement
• ヂスベリ ウンドウ ノ チシツガクテキ カイメイ ヤマガタケン タテ ノ サワ ヂスベリチ オ レイ ト シテ
• as an example of the Tatenosawa landslide in Yamagata Prefecture, Northeastern Japan
• 山形県楯ノ沢地すべり地を例として

抄録

Some sediments (sandy soil and black soil layers) of head of the landslide block were investigated, which appeared by road construction. After landslide movement, sandy soil sediments filled on an irregular surface and black soil deposited continuously on a flat slope. These depositions increase the load and caused next landslide, which repeated several times. The IIIA slide block makes a synchronous development with advance toward an old stage of geographical cycle . A preventive policy of this landslide was planned on the base of interpretation of historic change of this landslide.

収録刊行物

• 地すべり

  地すべり 39 (3), 307-318, 2002

  公益社団法人 日本地すべり学会

キーワード

• 地すべり堆積物
• 黒土
• 老年期
• 地形の輪廻
• 歴史的変遷

詳細情報

• CRID: 1390001204545059840
• NII論文ID: 10010212470
• NII書誌ID: AN00332562
• DOI: 10.3313/jls1964.39.3_307
• ISSN: 18843956
• ISSN: 02852926
• NDL書誌ID: 6417689
• Web Site: http://id.ndl.go.jp/bib/6417689
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I6417689
• データソース種別:
  • JaLC
  • NDL
  • Crossref
  • CiNii Articles
• 抄録ライセンスフラグ: 使用不可