Skip to main content

Science – Society – Technology

Fig. 10 | Geothermal Energy

Fig. 10

From: 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 play

Fig. 10

Hydraulic and thermal effect of the Inn Glacier (i.e. difference between model runs E and C introduced in Fig. 3). a Hydraulic head difference and b temperature difference induced by the Inn Glacier at its maximum extent 26.3 ka ago (time = 1.037E5 a) in the high Malm permeability scenario under paleoclimatic conditions. Vertical exaggeration equals three

Back to article page