Geologic clarifications of a landslide movement

DOI Web Site 3 Citations 11 References
  • YAMANOI Tohru
    Department of Earth and Environmental Sciences, Faculty of Science, Yamagata University

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Other Title
  • 地すべり運動の地質学的解明
  • 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

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Description

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.

Journal

  • Landslides

    Landslides 39 (3), 307-318, 2002

    The Japan Landslide Society

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