Fig. 6From: Examination of an active submarine fault off the southeast Izu Peninsula, central Japan, using field evidence for coseismic uplift and a characteristic earthquake modelDistribution of inferred mean coseismic uplift and the offshore fault at the southern end of the Izu Peninsula. a Bathymetric map. b Red-relief image map off Shimoda area (Asia Air Survey, Japan). Deep red indicates steep slope and light red indicates flat surface (Chiba et al. 2008)Back to article page