Recurrence Interval of Slope Failures and Debris Flows Caused by Heavy Rainfall in Mountain Slope in Japan
Author:
Affiliation:
1. Institute of Socio-Arts and Sciences, University of TOKUSHIMA
2. Storm, Flood, and Landslide Research Unit, Observation and Prediction Research Division, National Research Institute for Earth Science and Disaster Prevention
Publisher
Japan Society of Engineering Geology
Reference32 articles.
1. About the "Immunity" of the Disaster in Mountainous Area
2. Chronology of mass movement and slope formation in the central Kitakami Mountains, northeast Japan.
3. Landform development during the Last Glacial and the Post-Glacial Ages in the Matsumoto Basin and its surrounding mountains, Central Japan.
4. Vertical change of slope stability from Last Glacial to early Holocene in the southern part of the Yubari mountains and the western part of the Hidaka range, Hokkaido, Japan.
5. Period of Piedmont Gentle Slope Formation since the Last Interglacial in the Northern Part of the Kitakami Mountains, Northeastern Japan.
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2. Debris Flow Behaviors During the 2018 West Japan Rainstorm Disaster;Journal of the Japan Society of Engineering Geology;2023-04-10
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4. Immunity to Slope Failures Based on Their Distribution Induced by the 1945 Makurazaki Typhoon and 2018 Heavy Rainfall;Geographical review of Japan series A;2022-03-01
5. A SLOPE FAILURE TYPE CLASSIFICATION ALGORITHM FOR MULTIPLE SIMULTANEOUS SLOPE FAILURE HAZARD ASSESSMENT;Journal of Japan Society of Civil Engineers, Ser. F3 (Civil Engineering Informatics);2020
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