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Titlebook: GIS Landslide; Hiromitsu Yamagishi,Netra Prakash Bhandary Book 2017 Springer Japan KK 2017 Digital Elevation Model.GIS Landslide Workshop.

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Characteristics of the Torrential Rainfall-Induced Shallow Landslides by Typhoon Bilis, in July 2006ensity rainfall was the major triggering factor. In addition, topographical factors such as slope and aspect also contributed to landslide occurrence. The combined influence of rainfall and the topographic factors.  The paper attempts to provide a better understanding of the rainfall and causative f
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Book 2017he workshop has significantly contributed to progress in the field..Included among the chapters of this book are GIS using susceptibility mapping, analyses of deep-seated and shallow landslides, measuring and visualization of landslide distribution in relation to topography, geological facies and st
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Identification and Mapping of Landslidesain scarps, debris, mounds, and hollows, or shallow landslides. Deep-seated landslides are classified into rotational slide (slump), planar slide (glide), debris avalanche, or earth flows. Shallow landslides are composed of scar, flow, and deposit part. The seat is classified into planar or spoon ty
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Spatial Comparison of Two High-resolution Landslide Inventory Maps Using GIS—A Case Study of the Augated using high-resolution ortho-photoimagery and a 2-m DEM. We found that the number of the August 1961 landslides is more than twice the July 2004 landslides. More than half of the July 2004 landslides (about 70% as the number ratio and 54% as the area ratio) were primary landslides. These primary
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Landslide Surface Deformation Detected by Synthetic Aperture Radar (SAR) Interferometry in Shizu Are suitable for observing landslide surface deformation in Japan. In this study, we produced InSAR (SAR interferometry) images using PALSAR data and observed the fringes produced; after subtracting orbital and topographic fringes, the resulted fringe indicated a 2 × 1 km landslide surface deformation
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