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Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: Evaluating variability in coseismic slips of paleoearthquakes from an incomplete slip history: an example from displaced terrace flights across the Kamishiro fault, central Japan

Fig. 2

Seismic intensity of the 1714 and the 2014 earthquake. Intensity is shown in Japan Meteorological Agency scale (0–7). The intensity and the epicenter of the 1714 event were from Tsuji (2003), and those of the 2014 earthquake were from the Geological Survey of Japan (2014). Error of the 1714 epicenter was within a 25 km radius

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