Alpine Geology
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Alpine Geology
The Alps form part of a Cenozoic orogeny, orogenic belt of mountain chains, called the Alpide belt, that stretches through southern Europe and Asia from the Atlantic Ocean, 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 from the Carpathian Mountains, Carpathians to the east. Orogeny took place continuously and tectonics, tectonic subsidence has produced the gaps in between. The Alps arose as a result of the collision of the African plate, African and Eurasian plate, Eurasian Plate tectonics, tectonic plates, in which the Alpine Tethys, which was formerly in between these continents, disappeared. Enormous Compressive stress, stress was exerted on sediments of the Alpine Tethys basin and its Mesozoic and early Cenozoic Stratum, strata were pushed against the stable Eurasian landmass by the northward-moving African landmass. Most of this occurred during the ...
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Alps 2007-03-13 10
The Alps () ; german: Alpen ; it, Alpi ; rm, Alps ; sl, Alpe . are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately across seven Alpine countries (from west to east): France, Switzerland, Italy, Liechtenstein, Austria, Germany, and Slovenia. The Alpine arch generally extends from Nice on the western Mediterranean to Trieste on the Adriatic and Vienna at the beginning of the Pannonian Basin. The mountains were formed over tens of millions of years as the African and Eurasian tectonic plates collided. Extreme shortening caused by the event resulted in marine sedimentary rocks rising by thrusting and folding into high mountain peaks such as Mont Blanc and the Matterhorn. Mont Blanc spans the French–Italian border, and at is the highest mountain in the Alps. The Alpine region area contains 128 peaks higher than . The altitude and size of the range affect the climate in Europe; in the mountains, precipitation ...
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