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The surface geology of Germany has evolved to its current configuration due to regional differences in the action and appearance of external and internal forces during the last c. 20 million years. Germany can be divided into three physiographic regions: the Central European Depression, the Central European Blocks and the Alps.
57,485 km 2 (22,195 sq mi) General map of Germany. 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 Bohemian Massif is a province within the Hercynian Forest subsystem. It borders with four provinces: Western Carpathians on the east, Eastern Alps on the south, North European Plain on the north, and Central Uplands on the west.
Geology of the Alps. The Alps form part of a Cenozoic orogenic belt of mountain chains, called the Alpide belt, that stretches through southern Europe and Asia from the Atlantic all the way to the Himalayas. This belt of mountain chains was formed during the Alpine orogeny. A gap in these mountain chains in central Europe separates the Alps ...
The North German Basin located in western Europe, represented as the green region defined by USGS. The North German Basin is a passive-active rift basin located in central and west Europe, lying within the southeasternmost portions of the North Sea and the southwestern Baltic Sea and across terrestrial portions of northern Germany, Netherlands, and Poland.
Large parts of the Elbe Sandstone Mountains are under statutory protection. In Germany there is the national park region of Saxon Switzerland, which consists two elements: Saxon Switzerland National Park itself, founded in 1990 and covered an area of 93 km²; and the protected area surrounding it that was founded in 1956 and covers 287 km².
Hercynian Forest. The Hercynian Forest was an ancient and dense forest that stretched across Western Central Europe, from Northeastern France to the Carpathian Mountains, including most of Southern Germany, though its boundaries are a matter of debate. It formed the northern boundary of that part of Europe known to writers of Antiquity.
The Harz is the most geologically diverse of the German Mittelgebirge, although it is overwhelmingly dominated by base-poor rocks. The most common rocks lying on the surface are argillaceous shales, slaty (geschieferte) greywackes and granite intrusions in the shape of two large igneous rock masses or plutons.