Using an airborne laser scanner for the identification of shallow landslides and susceptibility assessment in an area of ignimbrite overlain by permeable pyroclastics |
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| Authors: | Masahiro?Chigira mailto:chigira@slope.dpri.kyoto-u.ac.jp" title=" chigira@slope.dpri.kyoto-u.ac.jp" itemprop=" email" data-track=" click" data-track-action=" Email author" data-track-label=" " >Email author,Fengjun?Duan,Hiroshi?Yagi,Takahiko?Furuya |
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| Affiliation: | (1) Disaster Prevention Research Institute, Kyoto University, , 611-0011 Gokasho, Uji, Japan;(2) Yamagata University, 1-4-12 Koshirakawa, 990-8560, Yamagata, Japan;(3) Chiba University, 1-33 Yayoi, 263-8522 Inage, Chiba , Japan |
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| Abstract: | ![]()
An airborne laser scanner can identify shallow landslides even when they are only several meters in diameter and are hidden by vegetation, if the vegetation is coniferous or deciduous trees in a season with fewer leaves. We used an airborne laser scanner to survey an area of the 1998 Fukushima disaster, during which more than 1,000 shallow landslides occurred on slopes of vapor-phase crystallized ignimbrite overlain by permeable pyroclastics. We identified landslides that have occurred at the 1998 event and also previous landslides that were hidden by vegetation. The landslide density of slopes steeper than 20° was 117 landslides/km2 before the 1998 disaster. This event increased the density by 233 landslides/km2 indicating that this area is highly susceptible to shallow landsliding. |
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| Keywords: | Laser scanner Landslide Rainstorm Susceptibility mapping Fukushima, Japan |
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