Fig. 6From: The interplay of Malm carbonate permeability, gravity-driven groundwater flow, and paleoclimate – implications for the geothermal field and potential in the Molasse Basin (southern Germany), a foreland-basin playEvolution of the Inn Glacier height in the Alpine foreland during the Würm Glaciation (see also Seguinot et al. 2018). Glacier height is applied as time-dependent hydraulic head at the southern model boundary (Inn Glacier in Fig. 4)Back to article page