Fig. 2From: Historical and paleo-tsunami deposits during the last 4000 years and their correlations with historical tsunami events in Koyadori on the Sanriku Coast, northeastern JapanTopography and geology around the Funakoshi Peninsula. Base map is based on the 5 m mesh DEM supplied by the Geospatial Information Authority of Japan. Geology is modified after Yoshida et al. (1984)Back to article page