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Table 1 Magnitude of the geodetic volume change in the deflation source (\(\Delta V_\text{G}\)), erupted magma volume (\(\Delta V_\text{E}\)), and \(\Delta V_\text{E}/\Delta V_\text{G}\) in the later period of lava effusion during the 2011 and 2018 Shinmoe-dake eruptions (shown by shaded ranges in Fig. 2)

From: Constraints on magma storage conditions based on geodetic volume change and erupted magma volume and application to the 2011 and 2018 eruptions at Kirishima Shinmoe-dake volcano, Japan

Year

Period

\(\Delta V_\text{G}\) (\(10^{6}\) m\(^{3}\))

\(\Delta V_\text{E}\) (\(10^{6}\) m\(^{3}\))

\(\Delta V_\text{E}/\Delta V_\text{G}\)

2011

22:36, Jan. 29–22:39, Feb. 1

3.87

10.40

2.69

2018

23:30, Mar. 6–23:16, Mar. 10

3.92

9.13

2.33