Fig. 3From: Numerical estimation of a tsunami source at the flexural area of Kuril and Japan Trenches in the fifteenth to seventeenth century based on paleotsunami deposit distributions in northern JapanPreviously proposed fault models used in this study. a The eight fault models of the historical tsunami (Aida 1977, 1978; Satake et al. 2008; Okamura and Namegaya 2011; Watanabe et al. 2012; Imai et al. 2015; Ioki and Tanioka 2016; Tohoku Electronic Power 2016). b One historical tsunami model (Yamanaka and Tanioka 2022), two disaster prevention models (Hokkaido Disaster Prevention Council 2012; Cabinet Office 2020), and modified previously proposed models (i.e., HEKT and Hidaka models). The color bar in b shows the slip amount of the Cabinet Office (2020) model. See Table 2 for details. The gray lines are bathymetric contour lines drawn at 1000Â m intervalsBack to article page