Earthquake
The earthquake was associated with areas of both uplift and subsidence. On both the Boso Peninsula and Miura Peninsula a clear paleo shoreline has been identified, indicating up to 5 m of uplift near Mera (about 8 km south of Tateyama) and up to 1.2 m of uplift on Miura, increasing to the south. This distribution of uplift, coupled with modelling of the tsunami, indicate that at least two and probably three fault segments ruptured during the earthquake.
Read more about this topic: 1703 Genroku Earthquake
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