Fig. 1.
From: Detection and mapping of soil liquefaction in the 2011 Tohoku earthquake using SAR interferometry
(a) The study area (black rectangle) overlaid on the Japan Meteorological Agency seismic intensity of the 2011 earthquake (based on Hoshiba et al., 2011). (b) The topography of the Kanto region and the analyzed scene. Two rectangles located on the waterfront along Tokyo Bay and the Tone River covered by the SAR data, with ascending and descending orbits. Main branch of the Tone River is shown by a black line. (c) A geomorphologic classification map of the Kanto region with about a 1-km mesh (based on Wakamatsu et al., 2005).