Skip to main content
Progress in Earth and Planetary Science
Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

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. 6

Computed inundation area at Sekinehama using fault models by previous studies. Comparison computed inundation area using previously proposed fault models (Fig. 3 and Table 2) with tsunami deposit distribution at Sekinehama: a 1611 CE Keicho tsunami model by Aida (1977), b 1611 CE Keicho tsunami model by Imai et al. (2015), c 1611 CE Keicho tsunami model by Yamanaka and Tanioka (2022), d seventeenth-century tsunami model by Satake et al. (2008), e seventeenth-century tsunami model by Ioki and Tanioka (2016), f seventeenth-century tsunami model by Okamura and Namegaya (2011), g Hokkaido Disaster Prevention model (2012), h Cabinet Office (2020) model (Case 2), i 1968 CE Tokachi-oki tsunami model by Aida (1978), j 1968 CE Tokachi-oki tsunami model by TEP (2016), k submarine active fault model by Watanabe et al. (2012), and l 1640 CE Mt. Komagatake eruption tsunami model by Nakanishi and Okamura (2019). The red circles show the sites where tsunami deposits possibly formed in the fifteenth to seventeenth century, found by Ishimura et al. (2022). The solid contour shows the topography, and the dotted contour shows the bathymetry (less than 0 m), and these contour intervals are 2 m

Back to article page