Quantitative assessment on the influence of heavy rainfall on the crystalline schist landslide by monitoring system -case study on Zentoku landslide, Japan

Author:

Hong Yong,Hiura Hiromasa,Shino Kazuo,Sassa Kyoji,Fukuoka Hiroshi

Publisher

Springer Science and Business Media LLC

Subject

Geotechnical Engineering and Engineering Geology

Reference6 articles.

1. Furaya G, Sassa K, Hiura H, Fukuoka H (1999) Mechanism of creep movement caused by landslide activity and underground erosion in crystalline schist, Shikoku Island, southwestern Japan. Eng Geol 53:311?325

2. Hiura H, Sassa K, Fukuoka H (1991) On the mechanism of a crystalline schist landslide: landslide movement and the underground erosion. In: The Soviet-China-Japan Symp. and Field Workshop on Natural Disasters, Shanghai, Lanchzou, Urumgi, Alma-ata, Dushanbe and Kazsalezashchita, USSR, pp 21?30

3. Sassa K (1984) Monitoring of a crystalline schist landslide: compressive creep affected by ?underground erosion?. In: Proceedings of 4th International Symposium on Landslide, Toronto, vol. 2, University Toronto Press, Downsview, pp 179?184

4. Sassa K, Takei A, Kobashi S (1980) The movement and the mechanism of a crystalline schist landslide ?Zentoku? in Japan. Proc. INTERPRAEVENT 1980, Bad Ischl, vol. 1, Forschungsgesellschaft für vorbeugende Hochwasser bekämpfung, Klagenfurt, pp 85?106

5. Sugawara N (1972) Analysis method of valley discharge. Kyoritsu Publisher, Tokyo, Japan (in Japanese)

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