いわゆる破砕帯地すべりの性格について

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From the view points of geology and geomorphology, the writer treated the so-called fractured zone type landslides, and pointed out their characters.<BR>The one is a large scale landslide caused by a certain character of deep-seated shear plane and tectonic movements, and has often a uphill-facing scarplets and double ridges at adjacent areas.<BR>The other occurs in the areas with Quaternary detrital deposits which is often originated from the large Scale landslides.
社団法人日本地すべり学会の論文