Schönfeld Upland
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Schönfeld Upland
The Schönfeld Upland (german: Schönfelder Hochland) is a plateau in Dresden. It is named after Schönfeld, the district of Dresden in the middle of the plateau. Up to 1950, when Pillnitz was incorporated into Dresden, the upland was known as the Pillnitzer Elbe Plateau. Location The Schönfeld Upland is in the east of the Saxon capital of Dresden. It extends over an area of approximately 45 square kilometres to the edges of neighbouring Dürröhsdorf-Dittersbach in the rural district of Sächsische Schweiz-Osterzgebirge. Places in the Schönfeld Upland include Borsberg, Cunnersdorf, Eichbusch, Eschdorf, Gönnsdorf, Helfenberg, Krieschendorf, Malschendorf, Pappritz, Reitzendorf, Rockau, Rosinendörfchen, Rossendorf, Schönfeld, Schullwitz, Weißig and Zaschendorf. The Dresden districts of Rochwitz, Oberwachwitz (where the Dresden TV Tower is located) and Bühlau are also part of the landscape of the Schönfelder Upland. The Schönfeld Upland is part of the West ...
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Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ...
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