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Fig. 3 | Progress in Earth and Planetary Science

Fig. 3

From: 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 Japan

Fig. 3

Previously 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 1000 m intervals

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