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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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https://doi.org/10.1007/978-3-031-43684-0uction of slope angle is mainly controlled by seismic acceleration amplitude, but also depends on particle arrangement and boundary effects. The proposed scaling law with an exponential decay well represents the relaxation process of surface slope in all experiments. Maximum velocities occur near th
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Second and Third Trimester Bleedingntury. Our subcommittee reviewed a large number of these historical documents and extracted information on the topographical and geological features of earthquake-induced landslides. The resulting database includes 130 landslide-events that occurred from the late prehistoric period to the 20th centu
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https://doi.org/10.1007/978-1-4842-9337-9hquakes 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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Implementation Opportunities and Challengesones 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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