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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.
The Rhenohercynian Zone or Rheno-Hercynian zone[2] in structural geology describes a fold belt of west and central Europe, formed during the Hercynian orogeny (about 350 to 280 million years ago). The zone consists of folded and thrust Devonian and early Carboniferous sedimentary rocks that were deposited in a back-arc basin along the southern ...
The Kupferschiefer (German for Copper Shale, also called Copper Slate) [1][2] or Kupfermergel (Copper Marl), (T1 or Z1) [3] is an extensive and remarkable sedimentary unit in Central Europe. The relatively monotonous succession is typically 30 to 60 centimetres (12 to 24 in) and maximum 2 metres (6.6 ft) thick, but extends over an area of ...
The geology of Europe is varied and complex, and gives rise to the wide variety of landscapes found across the continent, from the Scottish Highlands to the rolling plains of Hungary. Europe's most significant feature is the dichotomy between highland and mountainous Southern Europe and a vast, partially underwater, northern plain ranging from ...
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.
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.
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.
Major lithostratigraphic units of northwest Europe with the ICS 's geologic timescale of the Triassic. [1] The Germanic Trias Supergroup ( German: Germanische Trias-Supergruppe) is a lithostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of western and central Europe (north of the Alps) and the North Sea.