A report about the Caucasus Mountains, a majestic attraction and a highlight of the Caucasus, is presented in this article.

Message about the Caucasus Mountains

Caucasus mountains geographic location

They are spread between Asia and Europe, the Middle and Near East. The mountains of the Caucasian region are divided into 2 systems - the Lesser and Greater Caucasus. The Greater Caucasus is located almost to Baku from Taman and includes the Western, Central and Eastern Caucasus. But the Lesser Caucasus is mountain range near the Black Sea. They are located between the Black Sea and Caspian coasts, covering the territories of such countries as South Ossetia, Russia, Abkhazia, Armenia, Georgia, Turkey and Azerbaijan.

In translation, their name means "mountains hold the sky." Length Caucasus mountains is 1100 km, and their width is 180 km. The most famous and highest peaks of the system are Mount Elbrus and Kazbek.

How old are the Caucasus Mountains?

The Caucasian mountain system is the same age as the Alps and has a 30-million history inscribed in Greek myths and biblical lines. According to legend, when Noah released a dove from the ark in search of land, he brought a twig to Noah from the mountains of the Caucasian system. And the myths indicate that Prometheus, the man who gave fire to people, is chained here.

What do the Caucasus Mountains look like?

The mountains are fraught with many unusual things. On their peaks one can find preserved glaciation. Until now, earthquakes have been observed here, since the Caucasus Mountains are young from a geological point of view.

Their appearance is due to the relief, which is represented by different forms. Soared under the sky Mountain peaks with sharp peaks. With their outlines, they look like the walls of a castle with towers, then Egyptian pyramids. In the mountains there are also glaciers, rivers and areas with a surface heavily damaged by wind erosion.

Climate

The climate of the mountain system of the Caucasus is quite diverse. These places have a pronounced zonality. These mountains are a natural barrier that prevents the movement of air masses, thereby determining the diversity of the climate. The southern and western slopes receive much more precipitation than the northern and eastern slopes. The Caucasus Mountains are located in almost all climatic zones: from humid subtropics with wet and warm winters, dry hot summers to dry continental climate, turning into semi-desert in the east.

Near the foothills, snowy cold winters with dry summers are observed, and the higher the mountains, the lower the temperature. At an altitude of 3.5 thousand km. it reaches -4 0 C.

Flora and fauna

The mountains of the Caucasus are inhabited by unique animals. Among them are chamois, wild boars, mountain goats, foxes and bears, the Asia Minor mountain jerboa and ground squirrel, and in remote places ah bears and leopards live. On the way from the foot to the top, meadow alpine grasses and coniferous forests grow, which “feed” on rivers, lakes, waterfalls, mineral water springs.

• For the first time, a man climbed the highest peak of the Caucasus Mountains on July 22, 1829.
• There are a lot of invertebrate species in the Caucasus, for example, about 1000 species of spiders still live there.

  In the Caucasus 6349 species of flowering plants, including 1600 native species.

  In the Caucasus many endemic representatives- slightly less than 1600 species of flora, 32 species of mammals and 3 species of birds.

• Permafrost starts at altitude 3000-3500 m.

We hope that the report about the Caucasus Mountains helped you prepare for the lesson. And you can leave your message about the Caucasus Mountains through the comment form below.

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The Achishkho mountain range is the closest range to Krasnaya Polyana and the most picturesque. The highest mountain - Achishkho has a height of 2391 meters above sea level. Interesting fact about the name of the ridge: "Achishkho" in translation from the Abkhazian means "horse". This confirms the view from below, from Polyana to the mountain range. If you look closely, you can see the outline of a horse. The most popular hiking route passes through a special place located on the side of the mountain, approximately 1800 meters above sea level, where from the 30s to the 90s there was a weather station.

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The Aibga mountain range is located on the territory of Sochi national park, from the east side of Krasnaya Polyana. The ridge has a length of more than 20 kilometers, and consists of four highest points, called peaks. The most popular mountain peak among tourists is the Black Pyramid, 2375 meters above sea level. She has unusual shape which makes it very popular with climbers. In addition, a wonderful, breathtaking landscape opens up from the top of the mountain. Having conquered this mountain, you will see the valley of the Mzymta River, the peaks of Chugush and Pseashkho.

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One of the most beautiful resort places our country is Dombai. The main attractions of this city are its scenic spots. Mussa Ridge - Achitara is considered the most picturesque ridge of this part of the Caucasus. In order to appreciate all the beauty that surrounds the guests of the resort, you need to climb the slope of the mountain along cable car. This place offers a wonderful scenic view peaks and glaciers of the Main Range, Teberda and Gonachkhiri valleys.

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Peak Ine is located near the place where the northern Dzhugurlutchat glacier originates. The name of the mountain is translated as “Needle”, the mountain got its name because of its pointed top, this unusual view of mountains attracts many tourists from all over the world. The top of Ine Peak is covered with snow all year round, and although it sheer cliffs relatively difficult to conquer, the top of Ine Peak is quite a popular place for climbers. The height of the "needle" reaches 3455 meters, which is about 600 meters below the highest mountain of the Caucasus Dividing Range. It is best to view the mountain from the site of Mount Mussa-Achi-Tara, it is 400 meters lower than Ine Peak, but for that it can be reached by funicular.

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In the North Caucasus, among the Dombai glade, several east of the mountain Behind (Small) Belalakai there is a peak called Sufruju. The height of the mountain is 3871 m. A wide depression divides the massif into two equal parts - Southern and Northern. Both peaks are clearly visible from the ski Musat-Cheri. southern part They named the Tooth Sufruju, which means "Tiger's Fang". The massif stretches for 3600 m and acts as the main attraction of the mountain Dombai.

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Belalakai is a mountain located near the village in Dombay, since the village is a resort mountain has become a symbol of this village and attracts a lot of tourists. Its height is 3861 meters. Although the height of this mountain is 200 meters lower than the highest in Abkhazia, it is no less an attraction. Belalakai owes its fame to quartz. Most of the mountain consists of dark rocks of soil and dark granite, however, due to centuries of geological processes, there are deposits of quartz on the mountain. It is this quartz that has created the white streaks that adorn the top of this mountain, the white streaks of Belalakai are especially visible at the end of summer. Because of the beauty of the local landscapes, the mountain was mentioned more than once in songs and poems.

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Dzhuguturluchat is a relatively small massif, in the large Caucasian ridge. In height, the mountain range rose to 3921 meters, which is only 120 meters less than the highest point on the Caucasus Range. Herds of tours are found in the highest regions of the mountain range, it was they who gave these mountains the name "Dzhugurluchat" - which translates as: "herd of tours". The mountain range originates from the Dombai plateau, however, the most Beautiful places open from a place called "Mussa-Achi-Tara" is where most tourists gather.

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Cheget is one of the highest mountains in the Caucasus. Its height reaches about 3770 meters. This is popular place for tourism among travelers. From the mountain you can enjoy the view of the highest peak in Europe - Elbrus. Another feature of Mount Cheget is the second line of the cable car, which passes through the area where the snow lies, which does not melt throughout the year.There are three lines of the cable car in total. The height of the first reaches about 1600 meters. It is one of the most popular for tourists who come to Cheget to enjoy the view of Elbrus.

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This mountain after Elbrus is the second most popular among climbers. All because it is also quite high - 4454 meters above sea level.

There are several ways to get to the mountain by cable car or on foot. Tourists who have chosen the first method can use the Cheget cable car at the final point, where small cafes are located. The second and more difficult path, which takes several hours, is from the Cheget glade along a path already full of tourists. However, it is better to go on a journey with an experienced guide, otherwise there is a chance to get lost in the mountains.

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The North Caucasus will captivate many tourists with its beauties and landscapes. Mount Semyonov-Bashi, located in the east of the Caucasus Range, is no exception. In reality, this is just a ledge 3602 m above the ground. The mountain was named after the Russian explorer P.P. Semenov-Tyan-Shansky. This person was a traveler and was the chairman of the Russian Geographical Society.

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Mount Chotcha is part of the Caucasian ridge, which is famous for its picturesque mountains and rocks. Chotcha, unlike other mountains, is divided into two parts, as if someone cut the mountain in the middle into two halves. Unlike the mountains, which have just a smaller mountain nearby, at first glance it is clear that the mountain has one base on which there are two rocks. The rock in the foreground is lower than the back one, it has 3637 meters in height, it is 400 meters lower than the highest mountain of the Caucasian ridge. The second rock is only three meters higher than the first one, it is 3640 meters above sea level.

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Mount Ertsog is included in the list of one of the most visited places of the Caucasian ridge. At the foot of the mountain, the Alibek River flows, in addition to the mountain itself, this place has a very beautiful lowland. In the gorge where the river flows, a massive slope descends, it becomes especially beautiful in spring, when the sun illuminates the slope full of bright green vegetation. Mount Ertsog is part of the Teberdinsky ridge, the ridge itself encircles a lowland with a river and makes a very strong impression on tourists who visit it.

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Mount Sulohat is located in the Dombay region and is one of the most big dots Caucasian watershed range. The height of the mountain is 3439 meters, which is about 600 meters lower than the big mountain on the Caucasian ridge. Mount Sulohat is surrounded by many legends, the most popular one is about the origin of the name of the mountain. In ancient times, the foot of the mountain was inhabited by the Alans tribe. In this tribe lived a girl named Sulohat, she was extraordinary beauty and courage and was the daughter of the leader of the tribe.

Caucasian mountains

The Caucasus Mountains are located on the isthmus between the Caspian and Black Seas. The Kuma-Manych depression separates the Caucasus from the East European Plain. The territory of the Caucasus can be divided into several parts: Ciscaucasia, Greater Caucasus and Transcaucasia. In the territory Russian Federation located only Ciscaucasia and the northern part Greater Caucasus. The last two parts together are called the North Caucasus. However, for Russia, this part of the territory is the southernmost. Here, along the crest of the Main Range, passes state border Russian Federation, followed by Georgia and Azerbaijan. The entire system of the Caucasus Range occupies an area of ​​approximately 2600 m2, with its northern slope occupying about 1450 m2, while the southern one is only about 1150 m2.

The North Caucasian mountains are relatively young. Their relief was created by different tectonic structures. In the southern part there are folded-block mountains and foothills of the Greater Caucasus. They were formed when deep trough zones were filled with sedimentary and volcanic rocks, which were later subjected to folding. Tectonic processes here were accompanied by significant bends, extensions, ruptures and faults of earth layers. As a result, a large number of magma (this led to the formation of significant ore deposits). The uplifts that took place here in the Neogene and Quaternary periods led to the elevation of the surface and the type of relief that exists today. The rise of the central part of the Greater Caucasus was accompanied by the lowering of the layers along the edges of the ridge being formed. Thus, the Terek-Caspian trough was formed in the east, and the Indal-Kuban trough in the west.

Often the Greater Caucasus is presented as the only ridge. In fact, this is a whole system of various ridges, which can be divided into several parts. The Western Caucasus is located from the Black Sea coast to Mount Elbrus, then (from Elbrus to Kazbek) follows the Central Caucasus, and to the east from Kazbek to the Caspian Sea - the Eastern Caucasus. In addition, two ridges can be distinguished in the longitudinal direction: Vodorazdelny (sometimes called the main one) and Lateral. On the northern slope of the Caucasus, the Rocky and Pasture Ranges, as well as the Black Mountains, are distinguished. They were formed as a result of the interbedding of layers composed of sedimentary rocks of different hardness. One slope of the ridge here is gentle, and the other breaks off rather abruptly. As you move away from the axial zone, the height of the mountain ranges decreases.

The chain of the Western Caucasus begins at the Taman Peninsula. At the very beginning, it is rather not even mountains, but hills. They begin to rise towards the east. The highest parts of the North Caucasus are covered with snow caps and glaciers. The highest peaks of the Western Caucasus are the Fisht (2870 meters) and Oshten (2810 meters) mountains. The highest part of the mountain system of the Greater Caucasus is the Central Caucasus. Even some passes at this point reach a height of 3 thousand meters, and the lowest of them (Cross) lies at an altitude of 2380 meters. Here are the highest peaks of the Caucasus. So, for example, the height of Mount Kazbek is 5033 meters, and the two-headed dormant volcano Elbrus is indeed the highest peak in Russia.

The relief here is strongly dissected: sharp ridges, steep slopes and rocky peaks prevail. The eastern part of the Greater Caucasus is mainly made up of the numerous ranges of Dagestan (in translation, the name of this region means "mountainous country"). There are complex branching ridges with steep slopes and deep canyon-like river valleys. However, the height of the peaks here is less than in the central part of the mountain system, but still they exceed the height of 4 thousand meters. The uplift of the Caucasus Mountains continues in our time. Quite frequent earthquakes in this region of Russia are connected with this. To the north of the Central Caucasus, where the magma rising along the cracks did not spill onto the surface, low, so-called island mountains formed. The largest of them are Beshtau (1400 meters) and Mashuk (993 meters). At their base there are numerous sources of mineral waters.

The so-called Ciscaucasia is occupied by the Kuban and Tersko-Kuma lowlands. They are separated from each other by the Stavropol Upland, the height of which is 700-800 meters. The Stavropol Upland is dissected by wide and deeply incised valleys, gullies and ravines. At the base of this area lies a young slab. Its structure is made up of Neogene formations covered with limestone deposits - loess and loess-like loams, and in the eastern part there are also marine deposits of the Quaternary period. The climate in this area is quite favorable. Enough high mountains serve as a good barrier to cold air penetrating here. The proximity of the long cooling sea also has an effect. The Greater Caucasus is the border between two climatic zones - subtropical and temperate. On the Russian territory, the climate is still moderate, but the above factors contribute to rather high temperatures.

Mountains of the Caucasus As a result, winters in Ciscaucasia are quite warm ( average temperature in January is about -5°С). This is facilitated by those coming from outside Atlantic Ocean warm air masses. On the Black Sea coast, the temperature rarely drops below zero (the average January temperature is 3°C). AT mountainous areas the temperature is naturally lower. Thus, the average temperature in the plains in summer is about 25°C, and in the upper reaches of the mountains - 0°C. Precipitation in this area falls mainly due to cyclones coming from the west, as a result of which their amount gradually decreases towards the east.

Most precipitation falls on the southwestern slopes of the Greater Caucasus. Their number on the Kuban Plain is about 7 times lower. In the mountains of the North Caucasus, glaciation is developed, in terms of the area of ​​\u200b\u200bwhich this region ranks first among all regions of Russia. The rivers flowing here are fed by water formed during the melting of glaciers. The largest Caucasian rivers are the Kuban and Terek, as well as their numerous tributaries. Mountain rivers, as usual, are fast-flowing, and in their lower reaches there are swampy areas overgrown with reeds and reeds.

It is divided into two mountain systems: the Greater Caucasus and the Lesser Caucasus. The Caucasus is often divided into the North Caucasus and Transcaucasia, the border between which is drawn along the Main, or Watershed, ridge of the Greater Caucasus, which occupies a central position in mountain system. The Greater Caucasus stretches for more than 1100 km from the northwest to the southeast, from the Anapa region and Taman Peninsula to the Absheron Peninsula on the Caspian coast, near Baku. The Greater Caucasus reaches its maximum width in the region of the Elbrus meridian (up to 180 km). In the axial part is located the Main Caucasian (or Dividing) Range, to the north of which a number of parallel ranges (mountain ranges) extend, including a monoclinal (kuest) character (see Greater Caucasus). The southern slope of the Greater Caucasus mostly consists of echelon-shaped ridges adjacent to the Main Caucasian ridge. Traditionally, the Greater Caucasus is divided into 3 parts: the Western Caucasus (from the Black Sea to Elbrus), the Central Caucasus (from Elbrus to Kazbek) and the Eastern Caucasus (from Kazbek to the Caspian Sea).

Most famous peaks- Mt. Elbrus (5642 m) and Mt. Kazbek (5033 m) are covered with eternal snow and glaciers. The Greater Caucasus is a region with a large modern glaciation. The total number of glaciers is about 2050, their area is approximately 1400 km 2 . More than half of the glaciation of the Greater Caucasus is concentrated in the Central Caucasus (50% of the number and 70% of the glaciation area). Large centers of glaciation are Mount Elbrus and the Bezengi wall (with the Bezengi glacier, 17 km). From the northern foot of the Greater Caucasus to the Kuma-Manych depression, Ciscaucasia extends with vast plains and uplands. To the south of the Greater Caucasus are the Colchis and Kura-Araks lowlands, the Inner Kartli plain and the Alazan-Avtoran valley [the Kura depression, within which the Alazan-Avtoran valley and the Kura-Araks lowland are located]. In the southeastern part of the Caucasus - the Talysh mountains (up to 2477 m high) with the adjacent Lankaran lowland. In the middle and west of the southern part of the Caucasus is the Transcaucasian Highlands, consisting of the ranges of the Lesser Caucasus and Armenian highlands(Aragats city, 4090 m). The Lesser Caucasus is connected to the Greater Caucasus by the Likhi Ridge, in the west it is separated from it by the Colchis Lowland, in the east by the Kura Depression. The length is about 600 km, the height is up to 3724 m. The mountains near Sochi - Achishkho, Aibga, Chigush (Chugush, 3238 m), Pseashkho and others (Krasnaya Polyana resort area) - will host participants in the 2014 Winter Olympic Games.

Geology The Caucasus are folded mountains with some volcanic activity that formed as the Alps during the Tertiary Period (approximately 28.49-23.8 million years ago). The mountains are composed of, among other things, granite and gneiss, and contain deposits of oil and natural gas. Estimated reserves: up to 200 billion barrels oil. (For comparison: in Saudi Arabia- the country with the world's largest oil reserves - an estimated 260 billion barrels.) From a geophysical point of view, the Caucasus forms a wide deformation zone, which is part of the continental plate collision belt from the Alps to the Himalayas. The architectonics of the region was formed by the movement of the Arabian Plate to the north to the Eurasian Plate. Pressed by the African Plate, it moves every year by about a few centimeters. Therefore, at the end of the 20th century, large earthquakes with an intensity of 6.5 to 7 points occurred in the Caucasus, which had catastrophic consequences for the population and economy in the region. More than 25 thousand people died in Spitak in Armenia on December 7, 1988, about 20 thousand were injured and about 515 thousand were left homeless. Greater Caucasus - grandiose folded mountainous area, which occurred at the site of the Mesozoic geosyncline due to Alpine folding. Precambrian, Paleozoic and Triassic rocks lie in its core, which are successively surrounded by Jurassic, Cretaceous, Paleogene and Neogene deposits. In the middle part of the Caucasus, ancient rocks come to the surface.

Geographical affiliation There is no clear agreement on whether the Caucasus Mountains are part of Europe or Asia. Depending on the approach, high mountain Europe is considered respectively either Mount Elbrus (5642 m) or Mont Blanc (4810 m) in the Alps, on the Italian-French border. The Caucasus Mountains are located in the center of the Eurasian Plate between Europe and Asia. The ancient Greeks saw the Bosphorus and the Caucasus Mountains as the border of Europe. Later this opinion was changed several times for political reasons. During the Migration Period and the Middle Ages, the Bosphorus and the Don River separated the two continents. The border was defined by the Swedish officer and geographer Philipp Johann von Stralenberg, who proposed a border running through the peaks of the Urals and then down the Emba River to the coast of the Caspian Sea, before passing through the Kumo-Manych depression, which is 300 km north of the Caucasus Mountains. . In 1730, this course was approved by the Russian Tsar, and has since been adopted by many scholars. According to this definition, mountains are part of Asia and, according to this view, the highest mountain in Europe is Mont Blanc. On the other hand, La Grande Encyclopedie explicitly defines the border between Europe and Asia, south of both Caucasian ranges. Elbrus and Kazbek are European mountains by this definition.

Fauna and flora In addition to the ubiquitous wild animals, there are wild boars, chamois, mountain goats, as well as golden eagles. In addition, there are still wild bears. Extremely rare is the Caucasian leopard (Panthera pardus ciscaucasica), which was rediscovered only in 2003. In the historical period there were also Asian lions and Caspian tigers, but soon after the birth of Christ they were completely eradicated. A subspecies of the European bison, the Caucasian bison, became extinct in 1925. The last copy of the Caucasian elk was killed in 1810. There are a lot of invertebrate species in the Caucasus, for example, about 1000 species of spiders have been confirmed there so far. In the Caucasus, there are 6350 species of flowering plants, including 1600 native species. 17 species of mountain plants originated in the Caucasus. The giant Hogweed, considered in Europe as a neophyte of predatory species, comes from this region. It was imported in 1890 as an ornamental plant to Europe. The biodiversity of the Caucasus is declining at an alarming rate. The mountainous region is one of the 25 most vulnerable regions on Earth in terms of nature conservation.

Landscape The Caucasus Mountains have a varied landscape, which mostly varies vertically and depends on the distance from large bodies of water. The region contains biomes ranging from subtropical low-level swamps and glacier forests (Western and Central Caucasus) to high mountain semi-deserts, steppes and alpine grasslands in the south (mainly Armenia and Azerbaijan). Oak, hornbeam, maple, and ash are common on the northern slopes of the Greater Caucasus at lower elevations, while birch and pine forests predominate on the higher elevations. Some of the lowest areas and slopes are covered with steppes and meadows. On the slopes of the Northwestern Greater Caucasus (Kabardino-Balkaria, Karachay-Cherkessia, etc.) they also contain spruce and fir forests. In the highland zone (about 2000 meters above sea level), forests predominate. Permafrost (glacier) usually starts at about 2800-3000 meters. On the southeastern slope of the Greater Caucasus, beech, oak, maple, hornbeam and ash are common. Beech forests tend to dominate at higher altitudes. On the southwestern slope of the Greater Caucasus, oak, beech, chestnut, hornbeam and elm are common at lower altitudes, coniferous and mixed forests (spruce, fir and beech) at higher altitudes. Permafrost begins at an altitude of 3000-3500 meters.

Surprisingly beautiful mountain landscapes can be seen in these wonderful and unique places. The most impressive peaks are the Greater Caucasus Range. This is the territory of the highest and largest mountains in the Caucasus region.

The Lesser Caucasus and the valleys (Riono-Kura depression) represent Transcaucasia in the complex.

Caucasus: general description

The Caucasus is located between the Caspian Sea and the Black Sea in southwestern Asia.

This region includes the mountains of the Greater and Lesser Caucasus, as well as the depression between them called the Riono-Kura depression, the coasts of the Black and Caspian seas, the Stavropol upland, a small part of the Caspian lowland (Dagestan) and the Kuban-Azov lowland to the left bank of the Don River on part of its mouth.

The mountains of the Greater Caucasus have a length of 1500 kilometers, and the highest peak is Elbrus. The length of the Lesser Caucasus Mountains is 750 km.

A little lower, let's take a closer look at the Caucasus Range.

Geographical position

In the western part, the Caucasus borders on the Black and Seas of Azov, in the east - with the Caspian. In the north, the East European Plain extends, and the border between it and the Caucasian foothills repeats the latter passes along the river. Kuma, the bottom of the Kumo-Manychskaya depression, along the Manych and Vostochny Manych rivers, and then along the left bank of the Don.

The southern border of the Caucasus is the Araks River, behind which are the Armenian and Iranian Highlands, and the river. Chorokh. And already beyond the river, the peninsulas of Asia Minor begin.

Caucasian Range: description

The most courageous people and climbers have long chosen the Caucasian mountain range, which attracts extreme people from all over the world.

The most important Caucasian ridge divides the entire Caucasus into 2 parts: Transcaucasia and the North Caucasus. This mountain range extends from the Black Sea to the shores of the Caspian Sea.

The length of the Caucasus Range is more than 1200 kilometers.

The site, located on the territory of the reserve, is represented by the highest mountain ranges Western Caucasus. Moreover, the heights here are the most diverse. Their marks vary from 260 to more than 3360 meters above sea level.

The perfect combination of mild mild climate and amazing landscapes make this place ideal for active tourist holiday in any season.

The main Caucasian ridge on the Sochi territory has the largest peaks: Fisht, Khuko, Lysaya, Venets, Grachev, Pseashkho, Chugush, Malaya Chura and Assara.

The composition of the rocks of the ridge: limestones and marls. There used to be an ocean floor here. Throughout the huge massif, one can observe a pronounced folding with numerous glaciers, turbulent rivers and mountain lakes.

About the height of the Caucasus Range

The peaks of the Caucasus Range are numerous and quite diverse in height.

Elbrus is the highest point of the Caucasus, which is the highest peak not only in Russia, but also in Europe. The location of the mountain is such that a variety of nationalities live around it, giving it their unique names: Oshkhomakho, Alberis, Yalbuz and Mingitau.

The most main mountain in the Caucasus, it ranks fifth on Earth among mountains formed in a similar way (as a result of a volcanic eruption).

The height of the most gigantic peak in Russia is five kilometers six hundred and forty-two meters.

More details about the highest peak of the Caucasus

The most high altitude The Caucasian ridge is Russia. It looks like two cones, between which (a distance of 3 km from each other) at an altitude of 5200 meters there is a saddle. The highest of them has, as already noted, a height of 5642 meters, a smaller one - 5621m.

Like all peaks of volcanic origin, Elbrus consists of 2 parts: a 700-meter pedestal of rocks and a bulk cone (1942 meters) - the result of a volcanic eruption.

The peak is covered with snow starting from a height of about 3500 meters. In addition, there are glaciers, the most famous of which are the Small and Big Azau and Terskop.

The temperature at the high point Elbrus is -14 °C. Precipitation here almost always falls in the form of snow and therefore the glaciers do not melt. Due to the good visibility of Elbrus peaks from different remote places and at different times of the year, this mountain still has interesting name- Little Antarctica.

It should be noted that for the first time east summit was conquered by climbers in 1829, and the western one - in 1874.

Glaciers located on the top of Elbrus feed the Kuban, Malka and Baksan rivers.

Central Caucasus: ridges, parameters

Geographically, the Central Caucasus is part of the Greater Caucasus, located between the mountains of Elbrus and Kazbek (in the west and in the east). In this section, the length of the Main Caucasian Range is 190 kilometers, and if we take into account the meanders, about 260 km.

The border of the Russian state passes through the territory of the Central Caucasus. Behind it are South Ossetia and Georgia.

22 kilometers west of Kazbek ( East End Central Caucasus), the Russian border shifts slightly to the north and runs to Kazbek, skirting the Georgian valley of the Terek River (upper part).

On the territory of the Central Caucasus, 5 parallel ridges are distinguished (oriented along the latitudes):

1. The main Caucasian ridge (height up to 5203 m, Mount Shkhara).
2. Ridge Lateral (height up to 5642 meters, Mount Elbrus).
3. Ridge Rocky (height up to 3646 meters, Mount Karakaya).
4. Ridge Pastbishchny (up to 1541 meters).
5. Ridge Wooded (height 900 meters).

Tourists and climbers mainly visit and storm the first three ridges.

North and South Caucasus

The Greater Caucasus, as a geographical object, originates from the Taman Peninsula, and ends in the region. All subjects of the Russian Federation and countries located in this region belong to the Caucasus. However, in terms of the location of the territories of the constituent entities of Russia, there is a certain division into two parts:

• The North Caucasus includes Krasnodar region and Stavropol, North Ossetia, Rostov region, Chechnya, the Republic of Adygea, Ingushetia, Kabardino-Balkaria, Dagestan and Karachay-Cherkessia.
• South Caucasus (or Transcaucasia) - Armenia, Georgia, Azerbaijan.

Elbrus region

The Elbrus region is geographically the westernmost section of the Central Caucasus. Its territory covers the upper reaches of the Baksan River with its tributaries, the area north of Elbrus and the western spurs of Mount Elbrus to the right bank of the Kuban. most big top of this region and is the famous Elbrus standing to the north and located in the Lateral Range. The second highest peak is (4700 meters).

The Elbrus area is famous for a large number of peaks with steep ridges and rocky walls.

The largest glaciers are concentrated in the huge Elbrus glacier complex, which has 23 glaciers ( total area- 122.6 sq. km).

Location of states in the Caucasus

1. The Russian Federation partially occupies the territory of the Greater Caucasus and its foothills from the Dividing and Main Caucasian Ranges to the north. 10% of the total population of the country lives in the North Caucasus.
2. Abkhazia also has territories that are parts of the Greater Caucasus: the area from the Kodori to the Gagra ranges, Black Sea coast between the river Psou and Enguri, and to the north of Enguri a small part of the Colchis lowland.
3. South Ossetia is located in central area Greater Caucasus. Territory Start - Main Caucasian Range. The territory extends into southbound from it, between the Rachinsky, Suramsky and Lomissky ranges, to the very valley of the Kura River.
4. Georgia has the most fertile and populated parts of the country in the valleys and lowlands between the Lesser and Greater Caucasus ranges to the west of the Kakheti range. The most mountainous parts of the country are Svaneti, a section of the Greater Caucasus between the Kodori and Suram ranges. The Georgian territory of the Lesser Caucasus is represented by the Meskheti, Samsar and Trialeti ranges. It turns out that the whole of Georgia is within the Caucasus.
5. Azerbaijan is located between the Dividing Range in the north and the Araks and Kura rivers in the south, and between the Lesser Caucasus and the Kakheti Range and the Caspian Sea. And almost all of Azerbaijan (the Mugan Plain and the Talysh Mountains belong to the Iranian Highlands) is located in the Caucasus.
6. Armenia has part of the territory of the Lesser Caucasus (slightly east of the Akhuryan River, which is a tributary of the Araks).
7. Turkey occupies the southwestern section of the Lesser Caucasus, representing 4 eastern provinces of this country: Ardahan, Kars, partly Erzurum and Artvin.

The mountains of the Caucasus are both beautiful and dangerous. According to the assumptions of some scientists, there is a possibility that in the next hundred years the volcano (Mount Elbrus) may wake up. And this is fraught with catastrophic consequences for neighboring regions (Karachay-Cherkessia and Kabardino-Balkaria).

But, whatever it may be, the conclusion follows that there is nothing more beautiful than the mountains. It is impossible to describe all the magnificent nature of this fabulous mountain country. To feel it all, you should visit these amazingly beautiful paradise places. They are especially impressively viewed from the heights of the peaks of the Caucasus Mountains.