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Mountain system at the crossway of Europe, Asia, and the Middle East Caucasus MountainsAerial view of the Caucasus MountainsHighest pointPeak5,642 m (18,510 ft) DimensionsLength1,200 km (750 mi) Width160 km (99 mi) GeographyTopographic map CountriesArmenia, Azerbaijan, Georgia, Iran, Russia and TurkeyContinentCoordinates: Satellite image of the Caucasus Mountains The Caucasus Mountains are a mountain system at the crossway of Europe and Asia.
The Caucasus Mountains consist of the Greater Caucasus in the north and Lesser Caucasus in the south. winward casino. The Greater Caucasus runs west-northwest to east-southeast, from the Caucasian Natural Reserve in the vicinity of Sochi, Russia on the northeastern coast of the Black Sea nearly to Baku, Azerbaijan on the Caspian Sea.
The Greater and Lesser Caucasus varieties are linked by the Likhi Variety, and to the west and east of the Likhi Range lie the Colchis Plain and the Kur-Araz Lowland. The Meskheti Range belongs of the Lesser Caucasus system. In the southeast the Aras River separates the Lesser Caucasus from the Talysh Mountains which straddle the border of southeastern Azerbaijan and Iran.
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Mountains near Sochi hosted part of the 2014 Winter Olympics. winward casino. Geologically, the Caucasus Mountains belong to the Alpide belt system that extends from southeastern Europe into Asia and is thought about a border between the 2 continents. The Greater Caucasus Mountains are mainly composed of Cretaceous and Jurassic rocks with the Paleozoic and Precambrian rocks in the greater regions.
On the other hand, the Lesser Caucasus Mountains are formed predominantly of the Paleogene rocks with a much smaller sized portion of the Jurassic and Cretaceous rocks. The evolution of the Caucasus began from the Late Triassic to the Late Jurassic throughout the Cimmerian orogeny at the active margin of the Tethys Ocean while the uplift of the Greater Caucasus is dated to the Miocene throughout the Alpine orogeny. winward casino.
As the Tethys Sea was closed and the Arabian Plate clashed with the Iranian Plate and was pushed against it and with the clockwise movement of the Eurasian Plate towards the Iranian Plate and their last crash, the Iranian Plate was pressed against the Eurasian Plate. As this taken place, the whole rocks that had actually been deposited in this basin from the Jurassic to the Miocene were folded to form the Greater Caucasus Mountains.
The whole region is regularly subjected to strong earthquakes from this activity. While the Greater Caucasus Mountains have a primarily folded sedimentary structure, the Lesser Caucasus Mountains are mainly of volcanic origin. The Javakheti Volcanic Plateau in Georgia and the surrounding volcanic varieties which extend well into main Armenia are some of the youngest functions of the region.