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An analysis of the nonlinear magma-edifice coupling at Grimsvötn volcano (Iceland)

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Academic year: 2021

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Figure

Figure 1. Map of the caldera complex of the Grimsvötn volcano, showing the location of the GFUM permanent GPS station (black triangle) on Grimsfjall and the rims of the Grimsvötn caldera (from Gudmundsson and Milsom [1997]).
Figure 3. Physical model used in this study [from Carrier et al., 2015]. A magma reservoir (radius a r , depth H r , and roof depth H ) embedded in a homogeneous isotropic elastic half-space (density
Figure 4. Daily rate of M ≥ M c = 1 . 3 earthquakes (smoothed on 10 earthquake windows) that occurred in the area defined by Figure 1, as a function of the cumulative number of these earthquakes
Figure 6. Model variables as a function of time from 1 December 2004 to 31 December 2011, computed for
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