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Fig. 1. | Earth, Planets and Space

Fig. 1.

From: Switching from seismic to seismo-acoustic harmonic tremor at a transition of eruptive activity during the Shinmoe-dake 2011 eruption

Fig. 1.

(a) Seismic and acoustic stations (SMN, KRS, EBS station (KITK), and a monitoring camera (Cam.), nearby S crater (the red triangle). The geodetic source volume of th moe-dake eruption is 8 –10 km beneath the solid star. (b) map of (a). From Cam. to A –D are the directions of topo marks used as the scale references in the image analyses. line follows a chain of craters generated by the previous er flank of Shinmoe-dake. The open star and circle indicate of the source of lava effusion and the degassing vent at t the lava, respectively (Nakada et al., 2013).

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