THE OBSERVATION OF INTERNAL STRAIN AT A SHATTERED ZONE TYPE OF LANDSLIDE AREAS

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  • 破砕帯地すべり地の地中歪観測の2・3の結果
  • ハサイタイ ジスベリ チ ノ チチュウ ヒズミカンソク ノ 2 3 ノ ケッカ

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Abstract

Now the landslide surface and the mechanism of a landslide are commonly discussed, based on surveys by means of the internal strain meter. On case of a shattered zone typeof landslide ares, however, the data gathered in this method have a strain value of unknownorigin and have many things unsolved. This time, therefore, the observation of undergrounddeformation was made with a pipe strain meter of ordinary type and an internal strain meterof insertion type at a shattered zone type of landslide areas; Yakuaji, Kuki snd Nishiikawa.It has proved helpful for finding where the landslide surface exists.

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