Fig. 14From: 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 tsunamiAges of prehistorical tsunami deposits in Shizuoka Prefecture reported in previous studies. Shimoda: Kitamura and Kobayashi (2014a), Minami-Izu: Kitamura et al. (2013b) and Kitamura and Kawate (2015), Shimizu: Kitamura and Kobayashi (2014b), Shizuoka: Kitamura et al. (2013b), Yaizu: Kitamura et al. (2015a), Osuga: Uchida (2002), Rokken-gawa: Fujiwara et al. (2013), Lake Hamana: Tsuji et al. (1998)Back to article page