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 6 6 8 0 2 4 8 0 4 6 2 2 8 0 4 3 7 0 4 7 0 6 0 6 9 3 1 4 8 1 3 1 1 2 2 2 3 3 4 4 4 38800 4 38800  !  !  !  !  5  8 5  !  9  ! 

  !  57

! 6    1  !     6 !! ! 0  !   !  !   ! 5   ! 7 !    ! Hennigsdorf      6

  ! !  56  7

  6 6  5 9

  6 6 8

 5 "   6

" Stolpe 6  6 ! 5 ! 5

! 5 4   6

 ! 5 Zepernick 6 ! 3  36400 ! 36400 ! 2   5  ! ! 54 4 ! ! 3 6 6

1     5 " 0 1

 3  3  

8 53 5 32 9

 52  5 8 ! 52  ! !  3   ! 1 !  5 ! 1  ! Geologic Atlas ! 3 !  7

!

 !    ! ! !  !  !   !! ! 5  ! 0 ! 51  ! ! !  of !   !  34000 3   34000 6 4  9       3 50 5   "    5     8 3 4 4  9  5  7 5   6  5 48  5

 5  4

 

    3  3   8  4 l 31600    31600 3 2   

 5  3   47 

a       Groundwater Levels 46    5   5 9 31   t 2     of Berlin    43 45 31      e    44    51 29200    5 29200

      0

!  4  !   3 4  ! 4   9 of the Main Aquifer and 2 k   !  58     !  4

 ! 2  4    8

 ! !    !     0   4  ! 3  ! 1    !    n 4   !   7 !   ! Valley Aquifer ! 5 !  7  4   !     0  !  a !   !  !!!! ! ! !!!!   ! ! !!   3  ! ! Tegel P  9  ! 9 ! ! 41  5

! ! " 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 ! !   !  !  -Hochfläche 5

!  !  4 3 0 Spandau ! ! 5

! 4 4  !   4 2 ! !   4  9  ! ! 2 ! !    !   ! 4 ! ! "! ! 9 ! ! ! r ! ! ! !  ! !   ! ! !   ! !   ! !! !  !    1 ! !  4 s     Legend        3   1   4      8

   c

   

24400  24400 Groundwater isolines in meter over sea level (Normalhöhennull (NHN))  8    2      0  4 4    7   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

    3 39       ! 8

  !  51  !    

   i   Panke valley aquifer

 3     1  50          n  37 45   

     

  3 Area of the Panke aquifer in Berlin       6 e  19600      19600

       44 

  35         In the Panke Valley, sand of the Weichselian glacial period and the Holocene          ! r      4 overlay the glacial drift of the Barnim-Plateau. They form an independent cohorent  !   3        !      aquifer with unconfined surface of groundwater. !       ! !  !         ! The widespread units of glacial drifts can be covered by sand that conduct groundwater. Nauener Platte    !       ! 4  !  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 ! -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 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.