Translation of "Norddeutsches tiefland" in English

Geographically, Germany can be divided into the north German lowlands, the central German uplands and the Alpine foothills with the Alps.

If you select a position in the North German Plain, the online service displays at point 6 the note "North German Plain".

The Lübbecke Loessland is a transitional region between the North German Plain and the Central Uplands.

The route then continues on into the North German Plain through the water meadows of the Leine to Hanover.

In the North German Plain, snow loads up to a multiple of the numerical values have been recorded in rare cases.

In the north German lowlands almost two thirds of forests exist on previously cultivated fields, meadows or heaths.

Lowland castles are naturally found on plains such as the North German Plain or in the Netherlands.

Here the Bomlitz forms what, for the North German Plain, is an unusual, very striking series of meanders with river banks up to 20 metres high.

Extremely low divides with heights of less than two metres are found on the North German Plain within the "Urstromtäler", for example, between Havel and Finow in the "Eberswalde Urstromtal".

The North European Plain ( or ), or Middle European Plain (, ) is a geomorphological region in Europe, mostly in Poland, Germany, Denmark and Netherlands (Low Countries).

In the north it takes in part of the north German plain, in the middle section there are the agriculturally valuable loess soils and in the south we find the hills of Lower Saxony rising to heights of around 500 metres In the Soiling range.

The Rhine, Ems, Weser, Elbe and Havel are the most important rivers which drain the North German Lowlands into the North Sea and created woods in their flood plains and folds, e.g. the Spreewald ("Spree Forest").

The natural region is located in the central part of the North German Plain, straddling the border between the states of Lower Saxony (only the county of Lüchow-Dannenberg) and Saxony-Anhalt (counties of Altmarkkreis Salzwedel, Stendal and Börde).

Important for the emergence of the Urstromtäler is the fact that the general lie of the land on the North German Plain and in Poland slopes down from south to north.

The northern half of the Reglerungsbezirk Is part of the north German plain and takes in sections of the Lüneburg heath and of the Aller basin.

Extremely low divides with heights of less than two metres are found on the North German Plain within the Urstromtäler, for example, between Havel and Finow in the Eberswalde Urstromtal.

The Rahden-Diepenau Geest is part of the Dümmer Geest Depression and thus belongs to the North German Plain, although they include foothills of the Central Uplands in the shape of the Stemmer Berge.

The forest exhibits a transition, both in its geology and in its plant and animal life, between the North German Plain and the Central Uplands.

From north to south Germany is divided into five regions with different topographical features: the North German Plain, the Central Upland Range, the terrace panorama of the southwest, the Alpine foothills in the south and the Bavarian Alps.

Recolonisation took place around 7,000 years ago from what is now Slovenia, via the Eastern Alps, the Danube valley and Bohemia into the North German Plain and from there via Denmark to southern Sweden.

From the North and Baltic Seas to the Alps in the south, Germany is geographically sub-divided into the North German Lowlands, the Mittelgebirge ridge, the Central Uplands in southwest Germany, the South German Alpine foothills, and the Bavarian Alps.