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On the Mechanism of Landslide in Volcanic Altered Area in the Region of Hakone Volcano (2)
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- Watari Masasuke
- Public Works Research Ins'itute
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- Sakai Atsuyuki
- Public Works Research Ins'itute
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- Nakaiima Akira
- Public Works Research Ins'itute
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- Tomita Toshiyasu
- Public Works Research Ins'itute
Bibliographic Information
- Other Title
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- 火山性地すべりの運動機構に関する研究 (II)
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Description
Mechanical characteristics and movement mechanism of landslides in the area Owakudani-Sounzan area have been analyzed by various methods, such as measurements with tiltmeters and extensometers, observations of ground water levels and tests of soil mechanics, etc. From these, the following conclusions have been obtained.<BR>1) On the slope, of which the materials are composed of greatly altered rocks and clay, small landslides are sometimes detected, but large ones scarcely.<BR>2) Small landslides are characterized by slope failure, and their movements are influenced by precipitation.<BR>3) Small landslides often occur unexpectedly, and it is difficult to foreknow them.
Journal
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- Landslides
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Landslides 3 (2), 34-46, 1967
The Japan Landslide Society
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Details 詳細情報について
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- CRID
- 1390282679521976960
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- NII Article ID
- 130001006352
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- ISSN
- 18843956
- 02852926
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- Data Source
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- JaLC
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed