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Progress in Earth and Planetary Science
Fig. 3 | Progress in Earth and Planetary Science

Fig. 3

From: 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 tsunami

Fig. 3

Inundation heights of tsunamis caused by historical earthquakes. Distribution of inundation (heights in meters) in the coastal areas around Suruga Bay and Enshu-nada, as presented by Hatori (1976) and Watanabe (1998) for a the 1707 Hoei earthquake and b the 1854 Ansei-Tokai earthquake

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