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Nauen Plateau
The Nauen Plateau ((ドイツ語:Nauener Platte)) is a low plateau in the German states of Brandenburg and Berlin. It rises above the surrounding countryside by an average of and is a largely contiguous upland area that was formed during the Saale and Weichselian glaciations. It consists predominantly of ground moraine deposits, partly overlain by gently rolling end moraine formations. Whilst the neighbouring regions of Zauche to the south, the Teltow to the southeast and the Barnim to the northeast have the same name as their geological formation, the cultural landscape on the Nauen Plateau bears the historical and regional name of Havelland. That said, the river country of the Havelland extends beyond the plateau to include the Havel valley and other lowland areas.
== Location ==
The Nauen Plateau lies in the central Mark and in the extreme west of the state of Berlin. Its northern boundary is formed by a glacial meltwater valley, the Berlin Urstromtal, and by the former marshlands of the Havelland Luch, now part of the West Havelland Nature Park. North of the ''luch'' is the smaller ridge of ''Ländchen Glien''. The Plateau's eastern boundary is formed by the Berlin-Potsdam chain of Havelsee lakes, which separates the Nauen Plateau here from the plateau of Teltow. After turning westwards at the Templiner See the Havel valley between Potsdam and Brandenburg an der Havel marks the boundary of the Nauen Plateau to the south and separates it from the Zauche region.
The Havel valley also borders the region to the west, where the river swings north again after passing through the Plauer See. Between Pritzerbe, part of the town of Havelsee, and Paulinenaue, the western boundary of the Nauen Plateau runs west of the Garlitz and Ribbeck Heaths and east of the bird reserve established for the great bustard.
Its entire area covers about . From west to east it measures around 45 kilometres and from north to south around 20 kilometres.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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