Fig. 5From: New hypothesis to explain Quaternary forearc deformation and the variety of plate boundary earthquakes along the Suruga–Nankai Trough by oblique subduction of undulations on the Philippine Sea PlateVertical movement along the southern coast of the Kii Mountains. a Location of survey sites shown by small squares with symbols and coseismic vertical movements during the 1944 and 1946 Showa earthquakes by black solid lines in meter. b Height distribution of the MIS 5e terrace (Yonekura 1968). Symbols at the bottom indicate locations shown in a. c Height distribution of emergent fossil assemblages. Symbols at the bottom indicate locations shown in a (revised from Shishikura et al. 2008). d Photo of a vertical slice from fossil assemblage shown in c. Red circles are positions of 14C age samples. White dotted lines indicate discontinuous boundariesBack to article page