茶臼山地すべり下部の変動様相と埋没谷

概要

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Land mass produced by the landslide activity often fills up the existing valleys and forms buried valleys.The erosive action of valleys after the formation of buried valleys is apparently different from the erosive process which was proceeding in the old valleys before landslide. The deformation aspects of land surface of the mountain side slopes surrounding the old valleys are also different from those before the formation of buried valleys. In this report, we shall study the association between the deformation aspects of slide land mass and buried valleys, based on research and investigation of inside structures of the Chausuyama landslide.
社団法人日本地すべり学会の論文