Lateral Range Explained

Lateral Range
Other Name:Боковой хребет / გვერდითი ქედი
Region Type:Federal subjects
Parent:Greater Caucasus
Period:Paleozoic
Range Coordinates:43°N 67°W
Length Km:1100
Length Orientation:ESE/WNW
Width Orientation:NNE/SSW
Highest:Mount Elbrus
Elevation M:5642
Map:Caucasus mountains#European Russia
Label Position:none

The Lateral Range is a mountain range in the Russian Federation and Georgia, with a very small part in Azerbaijan. The range is part of the Greater Caucasus.

Some swathes of the range are protected areas, under the Kabardino-Balkaria Nature Reserve and the North Ossetia Nature Reserve.[1] [2]

Geology

In its western part the range is composed of Paleozoic and Triassic sedimentary rocks, in its central part of Upper Proterozoic and Paleozoic crystalline schist and granite, and in its eastern part of Jurassic shale.

Geography

The Lateral Range is characterized by alpine landforms. It runs parallel to the northern side of the Main Caucasian Range, to the south of the Skalisty Range, along the Krasnodar Territory, Karachay-Cherkessia, Kabardino-Balkaria, North Ossetia, Ingushetia, Chechnya and Dagestan federal subjects of Russia, as well as the countries of Georgia and Azerbaijan.[3] The range consists of somewhat detached mountain massifs, separated by the upper reaches of the rivers flowing from the northern slopes of the Greater Caucasus. The Lateral Range extends from the upper course of the Laba River, a left tributary of the Kuban, in the west, to almost the eastern end of the mountain system. It is made up of two parts: The western one is bound by the valley of the Ardon, and the eastern is a prolongation of the Main Caucasian Range, the dividing range of the Caucasus. The latter coincides with the alignment of the highest peaks of the eastern half of the Greater Caucasus, including the 5642m (18,510feet) high Elbrus, the 5203m (17,070feet) high Dykhtau and the 5100m (16,700feet) high Pushkin Peak.[3]

On the non rocky slopes of the Lateral Range there are alpine meadows, and in the central part there are several glaciated areas. There are high mountain pastures in the lower parts below the glaciers.[4]

See also

External links

Notes and References

  1. https://zapovednik-kbr.ru/ Кабардино-Балкарский заповедник Kabardina-Balkarskiy zapavyednik
  2. http://zapovednik15.ru/ Заповедник.ru
  3. [Google Earth]
  4. Web site: Боковой хребет. Great Soviet Encyclopedia.