About: North German Plain   Sponge Permalink

An Entity of Type : owl:Thing, within Data Space : 134.155.108.49:8890 associated with source dataset(s)

The aria is roughly encompassed by Lower Saxon Hills, the Teutoburg Forest, the Wiehen Hills, the Weser Hills, Lower Saxon Börde, the Westphalian Lowland, the Rhenish Massif, the Eifel, Northeast Mecklenburg Lowland, the Oder Valley, Bergisches Land, the Sauerland, East Brandenburg Plateau, Westphalian Lowland or Basin, Schleswig-Holstein Upland, East Frisian Geest, Upper Lusatian Plateau, Lower Rhine Plain, the Harz mountains, Kyffhäuser, Central Saxon hill country, the Ore Mountains, Szczecin Lagoon and the northern coastline with the North Sea and Baltic Sea.

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  • North German Plain
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  • The aria is roughly encompassed by Lower Saxon Hills, the Teutoburg Forest, the Wiehen Hills, the Weser Hills, Lower Saxon Börde, the Westphalian Lowland, the Rhenish Massif, the Eifel, Northeast Mecklenburg Lowland, the Oder Valley, Bergisches Land, the Sauerland, East Brandenburg Plateau, Westphalian Lowland or Basin, Schleswig-Holstein Upland, East Frisian Geest, Upper Lusatian Plateau, Lower Rhine Plain, the Harz mountains, Kyffhäuser, Central Saxon hill country, the Ore Mountains, Szczecin Lagoon and the northern coastline with the North Sea and Baltic Sea.
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abstract
  • The aria is roughly encompassed by Lower Saxon Hills, the Teutoburg Forest, the Wiehen Hills, the Weser Hills, Lower Saxon Börde, the Westphalian Lowland, the Rhenish Massif, the Eifel, Northeast Mecklenburg Lowland, the Oder Valley, Bergisches Land, the Sauerland, East Brandenburg Plateau, Westphalian Lowland or Basin, Schleswig-Holstein Upland, East Frisian Geest, Upper Lusatian Plateau, Lower Rhine Plain, the Harz mountains, Kyffhäuser, Central Saxon hill country, the Ore Mountains, Szczecin Lagoon and the northern coastline with the North Sea and Baltic Sea. It was formed during the Pleistocene era by glacial advances of terrestrial Scandinavian ice sheets. The region is drained by rivers that flow northwards into the North Sea or the Baltic. The important rivers Rhine, Ems, Weser, Elbe and Havel drain water from the North German Lowlands into the North Sea. This created woods in the rivers' flood plains and folds like the Spreewald ("Spree Forest"). Only a small area of the North German Plain falls within the catchment area of the Oder and Neiße rivers which drain out into the Baltic. It has several distinctive salt marshes, tide-flats and tidal reed beds in the estuaries existed permanently in the tidal zone of the North Sea coast. Special micro-climates occur in bogs and heath-lands and, for example, in the Altes Land near Hamburg. The local variety of beach trees dominate in the remaining forested places, whilst other places have bountiful orchards. Human intervention caused the emergence of open heath such as the Lüneburg Heath and measures such as deforestation and the so-called Plaggenhieb (removal of the topsoil for use as fertiliser elsewhere) caused a wide impoverishment of the soil (AKA-Podsol). North-east Mecklenburg Lowland is also marshy in some coastal places to. The lowest points are low moorlands and old marshland on the edge of the ridge of dry land in the west of Schleswig-Holstein called the Wilster Marsh. It is 3.5 metres below sea level and prone to flooding in stormy weather. Similar terrain and depths are found in the north west of Lower Saxony at the Freepsum. 2.3 metres below sea level and prone to flooding in stormy weather. The highest points are the Vistula and Hall glaciation terminal moraines on the Fläming Heath which is 200 metres above sea level and the Helpt Hills which is 179 metres above sea level. It has a maritime to sub-maritime climate. Wilhelmshaven was during the cold war and still is Germany’s only deep-water port and its largest naval base. The benefits of the access by a deep water shipping channel were already recognised at the end of the 1950s with the construction of the port’s first oil tanker jetty. The Border checkpoint Helmstedt–Marienborn (German: Grenzübergang Helmstedt-Marienborn), named Grenzübergangsstelle Marienborn (GÜSt) (border crossing Marienborn) by the German Democratic Republic (GDR), was the largest and most important border crossing on the Inner German Border during the Cold War division of Germany. It was one of the Warsaw Pact's prime targets and a critical assess point for the Easter Bloc's invasion of West Germany. The civilian toll would have been immense since it has several major towns and cities like: Lübeck- Population: 210,577 (2012), Hamburg- Population: 1.799 million (2012), Münster- Population: 291,754 (2012) and Osnabrück- Population: 165,021 (2012) in W. Germany, and Magdeburg- Population: 232,364 (2012) and Schwerin - population is 91,583 (2013) and in E. Germany.
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