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Fig. 11 | Progress in Earth and Planetary Science

Fig. 11

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. 11

Columnar sections of the study sites on the Oya lowland of the southeastern Shizuoka Plain. a Aerial photograph of the study area (source: website of Geospatial Information Authority of Japan, http://maps.gsi.go.jp/#12/34.985566/138.420353). b Inundation area of the Ansei-Tokai tsunami, after Shizuoka Prefectural Government (2011). The base map is the Shizuoka Tobu 1:25,000 topographic published by the Geospatial Authority of Japan. c Prediction of the wave height of a level 2 tsunami. After Kitamura et al. (2013b) and Shizuoka Prefectural Government (2013)

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