Berlin Environmental Atlas

02.12 Groundwater Levels of the Main Aquifer and Panke Valley Aquifer (Edition 2005)

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Geology and Hydrogeology

The present shape of the earth’s surface in Berlin was predominantly the result of the Vistula Ice Age, the most recent of the three great quaternary inland glaciations. The most important morphological units are the Warsaw-Berlin Glacial Spillway with the Panke Valley in the neighbourhood with predominantly sandy-gravel deposits, and the Barnim Plateau in the north and the Teltow Plateau with the Nauen Plate in the south, which are covered in large part by the thick glacial till or boulder clay of the ground moraines (Fig. 5).

Figure 5
Fig. 5: Geological Outline Map of Berlin

The loose sediments dating from the tertiary and quaternary, and averaging approx. 150 m in thickness, are of special significance for the water supply and for the foundation soil. They form the freshwater stock from which all the drinking water and a large part of the process water of the city is drawn.
The tertiary rupelton clay layer beneath it is about 80 m thick, and constitutes a hydraulic barrier against the deeper saltwater tier (Fig. 6).

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Fig. 6: Hydrogeological Cross-Section of Berlin

Due to the alternation of aquifers and aquitards, the freshwater stock in the Berlin area is broken down into four separate hydraulic aquifers (Limberg, Thierbach 2002). The second aquifer, which is largely a Saale-glaciation-era aquifer, is known as the main aquifer, since it supplies the predominant share of the drinking water. The fifth aquifer is already in the saltwater tier under the saltwater stock.

The groundwater conditions in the main aquifer (aquifer 2) are shown in the isoline map in violet, as well as the Panke Valley aquifer (aquifer 1) in the north-western area of the Barnim Plateau in blue. Here the Panke Valley aquifer situated above the main groundwater aquifer, separated by the clay-layer of the ground moraine (Fig. 6 and 7).

Figure 7
Fig. 7: The Panke Valley aquifer (aquifer 1) is situated above the main aquifer (aquifer 2)

In the north-western area of the Barnim Plateau the ground moraines are that mighty that no main groundwater aquifer exists or the main groundwater aquifer occures only in a thickness of a few meters. For those areas of the Berlin city groundwater isolines are not displayed.

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