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Figure 1

From: Seismic background level (SBL) growth can reveal slowly developing long-term eruption precursors

Figure 1

Overview of the monitoring system and the eruption sequences at Shinmoe-dake. (a) A map of Kirishima volcanic group in southwestern Japan (the white square in the inset: Goole Earth, Data SIO. NOAA.U.S. Navy NGA GEBCO). The white triangles indicate Shinmoe-dake and Iwo-yama. The colored circles are seismic stations used in this study, and white markers show other seismic stations. The vertices of the black triangle are the GEONET stations calculating the areal strain43, which represents the deep inflation beneath the asterisk40. The star indicates the epicenters of deep low-frequency earthquakes, whose rate correlated with the inflation at the asterisk44. (b) A schematic representation of Shinmoe-dake eruption sequences34,41. The August 2008 phreatic eruption, minor phreatic eruptions, the main phase of the 2011 eruption, the end of the 2011 eruption, the 2017 eruption, the main phase of the 2018 eruption, the April 2018 phreatic eruption at Iwo-yama, and the end of the 2018 eruption. The purple, light-gray, and dark-gray clouds indicate phreatic, ash-forming, and vulcanian eruptions, respectively.

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