Fig. 10From: 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 tsunamiEstimated co-seismic vertical crustal displacement of the 1854 Ansei-Tokai earthquake along the Suruga Bay coast. Units are meters. Figure is after Ishibashi (1984) and Kitamura and Kobayashi (2014b)Back to article page