Fig. 8From: Examination of the largest-possible tsunamis (Level 2) generated along the Nankai and Suruga troughs during the past 4000 years based on studies of tsunami deposits from the 2011 Tohoku-oki tsunamiColumnar sections of the study sites at Minami-Izu and Kisami. Modified from Kitamura and Kawate (2015)Back to article page