Fig. 11From: Spatiotemporal behavior of a large-scale landslide at Mt. Onnebetsu-dake, Japan, detected by three L-band SAR satellitesmodified from Cruden and Varnes, 1996). Red and green arrows indicate surface movement of upper and lower portion of landslide, respectively. Blue line indicates radar line-of-sight direction. Incidence angle is set to be 39 degrees, as is the case of JERS-1 (Table 1)Geometric relationship between radar incidence angle and surface topography of rotational landslides (Back to article page