Search results
Results from the WOW.Com Content Network
The North German Plain or Northern Lowland [1] (German: Norddeutsches Tiefland) is one of the major geographical regions of Germany. It is the German part of the North European Plain . The region is bounded by the coasts of the North Sea and the Baltic Sea to the north, Germany's Central Uplands ( die Mittelgebirge ) to the south, by the ...
This page was last edited on 16 December 2016, at 23:34 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.
Germany's major natural regions - Level 1: dark red, 2: orange, and 3: violet; major landscape unit groups: thin violet - based on the BfL classification. This division of Germany into major natural regions takes account primarily of geomorphological, geological, hydrological, and pedological criteria in order to divide the country into large, physical units with a common geographical basis.
Main page; Contents; Current events; Random article; About Wikipedia; Contact us
North European Plain coloured in green. Topography of the North European Plain.. The North European Plain (German: Norddeutsches Tiefland – North German Plain; Mitteleuropäische Tiefebene; Polish: Nizina Ćrodkowoeuropejska – Central European Plain; Danish: Nordeuropæiske Lavland and Dutch: Noord-Europese Laagvlakte; French: Plaine d'Europe du Nord) is a geomorphological region in Europe ...
Germany (German: Deutschland) is a country in Central and Western Europe [3] that stretches from the Alps, across the North European Plain to the North Sea and the Baltic Sea. It is the second-most populous country in Europe after Russia , and is seventh-largest country by area in the continent.
The Weser-Aller Plains and Geest [1] (German: Weser-Aller-Flachland) is a natural regional unit of the North German Plain in Germany.It extends over most of the southern catchment of the Aller including the lower reaches of the Oker and Leine and is bounded in the west by the Middle Weser.
Thus the Southern Ridge (German: Südliche Landrücken) is a moraine of the Saale glaciation and the Northern Ridge (German: Nördliche Landrücken) is a moraine of the Weichselian glaciation. [5] The material of these sediments was picked up by the ice sheet on its way from Scandinavia to Central Europe and was deposited during the melting there.