Fig. 7From: InSAR analysis for detecting the route of hydrothermal fluid to the surface during the 2015 phreatic eruption of Hakone Volcano, JapanResult of the inversion estimating the open crack and deflation sill model. a Modeled surface displacements, and b residuals between model and observation for Pair I. c Modeled surface displacements, and d residuals between model and observation for Pair II. B and C indicate displacement areas mentioned in the text. KM and SU show the summits of Kamiyama and Sounzan, respectively. Offset parameters were 1.95 mm for Pair I and –9.20 mm for Pair II. The red line and blue rectangle show the estimated open crack and deflation sill, the parameters of which are listed in Table 3Back to article page