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Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: Elastostatic effects around a magma reservoir and pathway due to historic earthquakes: a case study of Mt. Fuji, Japan

Fig. 2

Close-up map of Mt. Fuji, showing fissure distributions and locations of low-frequency earthquakes. The orange solid triangle indicated the summit, the orange open triangle indicates Hoei-san (a flank volcano produced by the Hoei eruption), and the black thin lines are topographic contours at intervals of 1500 m. The thick gray line represents the dike plane assumed by Chesley et al. (2012). The southernmost point of this plane is located at 138° 49.68′ E, 35° 15.18′ N; the strike is N323° E; and the dike length is 13 km. The dashed red line illustrates the eruptive fissure pattern compiled by Takada et al. (2007). The blue diamonds indicate the epicenters of the low-frequency earthquakes (over magnitude 1) during 2000–2014, as determined by the Japan Meteorological Agency

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