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Estimating epikarst water storage by time-lapse surface-to-depth gravity measurements

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Academic year: 2021

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Figure

Figure 1. Topographic map (elevation in metres) with the three sites indicated.
Figure 2. Hydrogeological setting of Lamalou karst system on the Hortus plateau. Seoubio cave (SEOU) is indicated by a red dot;
Figure 4. Developed cross section and topography surrounding (a) Seoubio caves, after Boinet (2002), and (b) Besses caves
Figure 5. Histogram of residuals of the observed gravity differences versus the adjusted gravity differences at the (a) SEOU site and (b) BESS site for each measurements periods
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