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Titlebook: Earthquake-Induced Landslides; Proceedings of the I Keizo Ugai,Hiroshi Yagi,Akihiko Wakai Conference proceedings 2013 Springer-Verlag Berli

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The Classification and Features of Earthquake-Induced Landslides in the Worldhquakes in the world was performed through mining the case studies from published literatures and documents. The sampled landslides triggered by big earthquakes (say,. > 6.0) since 1900 exceeds 70, and most of them are located in China, Japan, Iran, Indonesia, India, Pakistan, the United States, Chi
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Relationship Between Geological Structure and Landslides Triggered by the 2007 Mid-Niigata Offshore ones occurred with many small-scale ones by the 2007 Mid-Niigata Offshore Earthquake in spite of their similar geology and topography [landslide-scale with apparent volume (the Japan Landslide Society, .); small-scale: 10.–10. m., middle-scale: 10.–10. m., large-scale: 10.–10.m.]. Some of them, howe
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Catastrophic Landslides of Pyroclastics Induced by the 2011 off the Pacific Coast of Tohoku Earthquan Shirakawa and Nakagawa, where 6+ and 6− seismic intensities of JMA scale were recorded, respectively. These landslides occurred on rather gentle slopes with 13° to 23° with sliding surfaces in the depths of 3 m to 9 m but had a high mobility, which is shown by apparent friction angles ranging from
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Counsel’s Advice to the Medical Expertrmation and break of landslide dams, (2) Post-seismic landslides, (3) Long-term degradation of mountainous forest watershed, (4) Isolated districts due to traffic disruption and functional decline of countermeasure works.
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Secondary Hazards Associated with Coseismic Landslidermation and break of landslide dams, (2) Post-seismic landslides, (3) Long-term degradation of mountainous forest watershed, (4) Isolated districts due to traffic disruption and functional decline of countermeasure works.
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