Of Berlin Groundwater Levels
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" 6 2 ! ! ! ! ! 3 in May 2010 ! ! ! 3 3 ! 3 3 8 ! ! 5 6 5 ! 4 7 5 ! ! ! ! ! ! ! ! ! ! ! 4 ! ! 4 ! ! 0 6 ! ! ! ! ! ! 5 ! 3 4 ! ! 3 3 ! ! ! 9 26800 ! ! 26800 ! ! ! 4 53 5 ! ! ! ! ! ! ! W ! ! 0 ! 3 ! ! ! ! 4 ! 4 ! ! ! 2 ! 3 5 ! 3 2 9 ! 0 ! 0 ! ! ! ! ! 3 ! ! ! ! 2 ! ! ! 2 2 2 ! ! ! 9 ! ! 7 ! 8 2 !! ! ! 8 ! ! 4 51 a ! 6 ! ! ! ! Barnim-Hochfläche 5 ! ! 4 3 0 Spandau ! ! 5 ! 4 4 ! 4 2 9 ! ! 4 ! ! 2 ! ! ! ! 4 ! ! "! ! 9 ! ! ! r ! ! ! ! ! ! ! ! ! ! ! ! !! ! ! 1 ! ! 4 s Legend 3 1 48 c 24400 24400 Groundwater isolines in meter over sea level (Normalhöhennull (NHN)) 8 2 0 4 47 h 39 Main aquifer Staaken " 38 46 32 3 37 31 - in areas with unconfined groundwater 0 3 9 a 2 6 30 2 45 9 35 0 Jungfernheide 27 3 u 3 2 3 3 4 9 26 <!! ! - in areas with confined groundwater ! !! ! 4 ! ! 4 !! 25 - 3 2 43 B 3 42 Area without main aquifer or with isolated main aquifer up to few meters thickness 1 22000 ! 22000 ! ! ! ! ! ! e ! 41 47 The city-wide main aquifer is mostly composed of sand and gravel arised from the 2 ! ! ! ! 9 ! ! ! ! Saalian ice-age. The surface of groundwater located in the glacial valley is widely ! ! ! ! ! ! r ! ! Tiefwerder ! unconfined whereas the surface of groundwater below the plateaus consisting of ! "! 2 40 8 46 glacial drift is often confined. ! l ! 52 3 39 ! 8 ! 51 ! i Panke valley aquifer 3 1 50 n 37 45 Area of the Panke aquifer in Berlin 36 e 19600 19600 44 3 5 In the Panke Valley, sand of the Weichselian glacial period and the Holocene ! r overlay the glacial drift of the Barnim-Plateau. They form an independent cohorent 4 ! 3 ! aquifer with unconfined surface of groundwater. ! ! ! ! ! The widespread units of glacial drifts can be covered by sand that conduct groundwater. Nauener Platte ! ! 4 Kaulsdorf! 2 ! ! ! 34 ! 3 ! 2 U " ! ! ! ! ! 4 ! 1 ! ! ! ! ! Groundwater measurement point main aquifer ! 4 4 3 ! ! 0 2 ! 2 3 8 r ! 9 0 ! 3 ! 9 2 Groundwater measurement point Panke aquifer ! 7 s 33 8 17200 2 38 17200 3 1 ! t Level measurement point at surface water 1 ! 37 3 ! ! ! 3 ! 3 r 3 Operative water work ! 2 36 L ! ! ! 0 ! ! 3 ! ! 9 !!!!! ! ! !!!!!! ! 2 o ! !! !! ! ! ! !! ! ! (in the water works Jungfernheide and Johannisthal ! ! ! ! ! ! Unoperative water work ! ! 3 ! ! ! 3 ! ! Wuhlhe! ide! 5 are no water containment in this time) 3 !! !! ! ! ! ! 1 !!!! ! ! !! 8 ! !! m!!! 2 !! ! ! " !!! ! !!! !! Active well gallery !!! ! 34 ! ! ! ! ! ! ! ! ! ! ! ! ! ! 3 t 3 Border of the water conservation zone ! ! ! ! ! 14800 ! ! ! 14800 ! ! ! ! 32 ! ! a ! ! ! Riemeisterfenn ! ! ! 31 ! ! ! ! ! Kladow ! ! ! 3 ! < 3 ! "! ! ! ! ! ! ! ! ! ! ! ! 0 ! ! 3 Geology ! ! !! l ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! Friedrichshagen ! ! ! !! ! ! ! ! !! ! ! !! ! ! ! ! !!! ! ! ! ! ! ! !! !! ! ! ! ! ! !! ! ! ! ! 29 ! ! ! ! ! !!! !!! ! !! 3 ! ! ! ! ! " !! ! ! ! ! ! 0 !! ! ! ! ! ! !! ! !! ! ! ! ! ! ! ! ! ! !! !! ! ! ! ! ! ! Water ! ! ! ! ! ! ! Johannisthal ! !! ! ! < !! ! ! !! ! !! !! ! !! ! ! ! H ! 3 ! Formation of 1 ! ! ! o ! !! l ! ! ! o 3 4 Muds, Peat lake and bog beds ! c ! ! ! ! e ! ! n ! ! ! ! ! ! e ! 12400 12400 ! ! ! ! ! ! ! ! Q ! 2 ! Fine- to Medium Sand Formation of dunes 2 ! ! 3 5 3 ! 3 ! ! ! ! u ! ! ! ! a ! W ! 3 ! ! ! ! ! t 0 ! 2 ! e ! ! ! e ! ! ! ! 6 ! r 3 ! i ! Beelitzhof ! n c 4 ! ! ! ! ! ! h ! a 5 2 " ! ! ! ! ! ! r s ! ! ! ! ! 3 ! " y P ! e ! Sand in the Valley Formation of glacial 3 ! 5 l l ! 3 ! ! Erkner e ! ! ! i a ! 3 6 3 2 2 ! ! ! ! i 2 valleys and side-valleys s 7 ! 9 n 3 t 1 2 3 ! o 8 0 ! ! G c ! ! e ! l ! ! a ! n ! ! ! c 3 3 ! ! ! e Till, Glacial Drift* i a l P Formation of plateaus e r i o 7 3 d 10000 10000 Melt-water Sands M 4 i 3 Kleinmachnow d 0 ! ! d 3 ! ! ! l T e ! Teltow-Hochfläche e - ! r O t " i l a i g r 5 Clay to Silt ("Rupelton")** Marine sedimentation 3 y o c e n e 3 0 3 0 3 8 Note: The geological situation is shown up to a depth of 5 m maximum. ! ! ! ! For a simple description only the main layer is shown in the case of several layers. 3 5 ! 3 1 ! The depiction on the map does not absolve from the duty of local investigations. 6 3 ! ! * On the plateaus there can be temporary suspended groundwater ("stratum water"). ! ! ! ! ** The little occurrence of clay ("Rupelton") is being to the north of Waidmannslust. 7600 ! ! ! 7600 ! 7 3 ! 8 3 ! ! ! Teltow ! ! Scale 1 : 50 000 " 3 6 3 3 3 5 2 3 Coordinate system of the state: Soldner-Berlin 3 3 Elevation in meter over sea level (NHN) 4 3 9 3 Eichwalde 3 7 3 5200 3 " 5200 2 3 Published by: Senate Department for Health, the Environment and Consumer Protection 3 8 3 4 3 9 Conception: II E 3 (Geology and Groundwater Management) 1 3 Rehbrücke Scientifical 3 Editing: Ulrike Hörmann and Alexander Limberg 5 " Cartographical Editing: Wolfhard Schröter 2 3 Data: 1727 groundwater measured data and 33 surface water 2800 2800 measured data from measurement net works of state groundwater 3 6 survey Berlin, water supply Berlin, water works Brandenburg and 3 state invironmental administration Brandenburg, May 2010 3 Based on the Geologic Sketch of Berlin 1 : 50 000, 2008, Senate Department for Health, 4 geologic maps: the Environment and Consumer Protection based on the Geologic Sketch of Berlin 3 and Surrounding 1 : 100 000, published by Regional Authorities for Geo Sciences 3 5 7 3 and Resources Brandenburg, in cooperation with the Senate Department for Urban Development and Environment Protection, Berlin, Dep. IV, Kleinmachnow and Berlin 1995 Based on the 6 3 topographic map: Overview map of Berlin 1 : 50 000, Senate Department for Urban Development, 2004 400 400 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 4 8 2 4 6 8 0 2 4 6 6 0 2 0 6 8 4 0 7 0 3 6 0 3 6 9 7 4 1 8 1 4 1 1 2 2 3 3 3 4 4 4 4 1 2 This map is copyright protected. Reprinting or any other form of reproduction only with prior permission..