The geology of the North Sea describes the geological features such as channels, trenches, and ridges today and the geological history, plate tectonics, and geological events that created them. The Alpine orogeny was the last of the three major phases of orogeny in Europe that made its geology. The evolution of the North Sea basin occurred through multiple stages throughout the geologic timeline. This belt of mountain chains was formed during the Alpine orogeny. Alpine orogeny, mountain-building event that affected a broad segment of southern Europe and the Mediterranean region during the Paleogene and Neogene periods (65.5 million to 2.6 million years ago).
The orogeny continued well into the Cretaceous and Early Cenozoic. The process continues currently in some of the Alpide mountain ranges. The Alpine orogeny or Alpide orogeny is an orogenic phase in the Late Mesozoic [1] (Eoalpine) and the current Cenozoic that has formed the mountain ranges of the Alpide belt. The Alpine orogeny produced intense metamorphism of preexisting rocks, crumpling of rock strata, and uplift accompanied by both normal and thrust faulting. They are the highest part of Bohemian Massif. The major feature that was created by this orogeny was deep-seated, thick-skinned deformation, with evidence of this orogeny found from Canada to northern Mexico, with the easternmost extent of the mountain-building represented by the Black Hills of South Dakota. All content on this website, including dictionary, thesaurus, literature, geography, and other reference data is for informational purposes only. The Western Carpathians are a mountain range and geomorphological province that forms the western part of the Carpathian Mountains.

[2] Sometimes other names occur to describe the formation of separate mountain ranges: for example Carpathian orogeny for the Carpathians, Hellenic orogeny for the Pindus, Altai orogeny for Altai Mountains or the Himalayan orogeny for the Himalayas. It consisted of parts of what is today Turkey, Iran, Afghanistan, Tibet, Shan–Thai, and Malay Peninsula. During the Late Miocene and Pliocene, the, His topics are the construction of Baltica--proto-Europe, the Lower Paleozoic growth of proto-Europe, the Caledonian orogeny, the expansion of Europe in the Upper Paleozoic, the Hercynian orogenic cycle, Europe in Mesozoic to mid-Cenozoic time, the, This fold-thrust belt groves by the continuing active collision of the Arabian plate with the continental blocks of Central Iran (Ahmadhadi et al., 2007); but had a main event during the, Precambrian to the Cenozoic-age sediments were affected by the, Even within Europe's heartland region of rocks deformed by the (early Tertiary), Earth crust of Lower Silesia was broken into numerous tectonic blocks, grabens and horsts during late, The Dora-Maira Massif (composed of very high-pressure metamorphic rocks), is of great importance for the study of the, Tectonically the area has been faulted into a patchwork of blocks, some of them overthrusting as a result of the, Dictionary, Encyclopedia and Thesaurus - The Free Dictionary, the webmaster's page for free fun content, Seismic dynamics in the Vrancea depression and the impact on landscapes and touristic area development, New results for Palaeozoic volcanic phases in the Prague Basin-magnetic and geochemical studies of Listice, Czech Republic, The Making of Europe: A Geological History, Automatic mapping of lineaments using shaded relief images derived from digital elevation model (DEM) in Erbil-Kurdistan, northeast Iraq, Geometry, structures and evolution of the western termination of the Alpine-Pyrenean Orogen reliefs (NW Iberian Peninsula)/Geometria, estructuras y evolucion de la terminacion occidental de los relieves del Orogeno Alpino-Pirenaico (NO Peninsula Iberica), Is the Sudetic Marginal Fault still active?
The Alpine orogeny produced intense metamorphism of preexisting rocks, crumpling of rock strata,

The Mauritanide mountain chain was compressed and folded at that time along the western margin of the West African craton from Morocco to Senegal. This is a list of articles related to plate tectonics and tectonic plates. In the watershed region lies… Read More

The two…. by the Appalachian-Hercynian orogeny (mountain-building event), which continued into the Permian Period. Volcanic activity in England, France, Iceland, and parts of Italy also occurred during the Alpine orogeny. The Alpine orogeny or Alpide orogeny is an orogenic phase in the Late Mesozoic [1] (Eoalpine) and the current Cenozoic that has formed the mountain ranges of the Alpide belt.These mountains include (from west to east) the Atlas, … Alpine folding resulted in new mountains, the most marked upheaval being that of the Nether-Polar Urals. Be on the lookout for your Britannica newsletter to get trusted stories delivered right to your inbox. It extends from the Queen Elizabeth Islands through Peary Land and along the east coast of Greenland. The Alpine orogeny (sometimes Alpide orogeny) is the building of mountain ranges in central and southern Europe and west Asia.This mountain-building phase started in the later Mesozoic era. It includes, from west to east, the major ranges of the Atlas Mountains, the Alps, the Caucasus Mountains, Alborz, Hindu Kush, Karakoram, and the majestic Himalayas. Bern/Stuttgart/Wien: Haupt Verlag.

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 page was last changed on 10 May 2019, at 18:42. Differential uplift occurred in the late Paleogene and Neogene. 2002. eds. Geologie der Alpen (in German). Rosenbaum G. and Lister G.S. The basement rock is divided between the Grenville Province and Superior Province. The geology of Germany is heavily influenced by several phases of orogeny in the Paleozoic and the Cenozoic, by sedimentation in shelf seas and epicontinental seas and on plains in the Permian and Mesozoic as well as by the Quaternary glaciations.


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