02.12 Groundwater Levels

Map Description

The main aquifer predominantly consists of sands and gravel of the Saale Ice Age. In the glacial valley, the groundwater surface is largely unconfined, while on the plateaus it may be confined under a layer of boulder marl. The Panke Valley, which contains a substantial autonomous groundwater reserve, is shaded here.

• More Information

Map Imprint

Conception:
Gruppe VIII E 3 Landesgeologie und Landesgrundwasserdienst

Data Processing and Map Production:
Alexander Limberg, Wolfhard Schröter

Completed:
May 2002

Geoportal

• to the map

• 02.12 Groundwater Levels

  PDF-Document (3.5 MB)