Fig. 6From: Perspectives of lignite post-mining landscapes under changing environmental conditions: what can we learn from a comparison between the Rhenish and Lusatian region in Germany?(above) Geological cross-section (SW–NE, see Fig. 5: A–A´) of the Rhenish lignite mining district with hydraulic conductivity of Tertiary and Quaternary deposits and main coal seams; (below, divided into two parts) geological cross-section (SW–NE, see Fig. 5: B–B´) of the Lusatian lignite mining district with Tertiary and Quaternary deposits; note the different horizontal and vertical scales of both profiles (sources: redrawn from [32, 33]. Draft: F. Lehmkuhl, T. Rüde, and D. StawinogaBack to article page