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- W4247154428 abstract "A number of Tertiary type landslides are distributed in the northern part of Nagano Prefecture. They have various kinds of topography. The topographies due to shallow layer landslides in mudstone zone are, in general, simple. In the area consisting of the alternation of mudstone, sandstone and pyroclastic rock, deep layer landslides usually occur and bring complicated topographies. And in the zone of basement rock crushed by faults, specialized landslides are apt to break out: the area composed of pyroclastic rock intruding along the faults and metamorphosed pyroclastic rock forms more complicated topographies.The topography of Shimizuyama sliding area is the object of consideration presented here. Shimizuyama landslide occurs along the Himekawa fault, one of the faults belonging to the Itoigawa-Shizuoka tectonic line. Its sliding area has a length of 2, 000m, a width from 300m to 500m, and an area of 70ha, totalled of five sliding blocks. The major landslide occurs in the zone whose basement rock is crushed by the Himekawa fault and developed in the same direction (from south to north) as that of the Himekawa fault. The mountain flank by the sliding is, generally, gentle (8%-20%), where occur landslides or collapes scarcely. The fluviatile terraces in steps in the neighborhoods of the sliding area are gradually deformed by the sliding. Shimizuyama sliding area is large in scale and its sliding surfaces are usually shallow; this is the difference with such a landslide that a large-scale rock sliding in old times has kept on sliding. Shimizuyama sliding area is formed by the repeated landslides." @default.
- W4247154428 created "2022-05-12" @default.
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- W4247154428 date "1974-01-01" @default.
- W4247154428 modified "2023-09-25" @default.
- W4247154428 title "An Aspect of Geomorphic Deformation due to Landslide" @default.
- W4247154428 doi "https://doi.org/10.5190/tga1948.26.108" @default.
- W4247154428 hasPublicationYear "1974" @default.
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