Fig. 6From: Time difference between the 1854 CE Ansei–Tokai and Ansei–Nankai earthquakes estimated from distant tsunami waveforms on the west coast of North AmericaNormalized root mean square (NRMS) and NRMS misfit between observed and simulated waveforms of the 1854 CE Ansei–Nankai tsunami at the San Francisco and San Diego tide gauge stationsBack to article page