Unlike the Lesser Caucasus, which fills the entire southwestern part of the Caucasus region with its highlands and chains.

The entire system of the Caucasus Range occupies an area of ​​approximately 2600 square meters. m, and its northern slope occupies about 1450 sq. m, while the southern one is only about 1150 sq. m.

The main ridge at its western end approaches Anapa on the Black Sea coast, and at its eastern end ends with Mount Ilkhi-Dag (1073 f.), NW of Baku.

The distance in a straight line between these points is about 1100 versts, but, due to meanders and bends, the Main Range extends, in the form of a continuous high watershed, for almost 1420 versts.

The width of the Caucasus Range in the western (slightly west of Elbrus) and eastern (Dagestan) parts is about 200 versts, in the central - about 90 versts; both extremities are strongly narrowed and represent (especially the western) an insignificant width.

The highest is the middle part of the ridge, between Elbrus and Kazbek (cf. height 11600 ft.), where its highest peaks are concentrated, of which Elbrus reaches 18470 ft. above ur. seas; east of Kazbek and west of Elbrus, the ridge drops, and more significantly in the second direction than in the first.

In general, in terms of height, the Caucasian Range significantly exceeds the Alps; it has no less than 15 peaks exceeding 12,000 ft., and more than 20 peaks above Mont Blanc, the highest peak in all of Europe. The advanced heights accompanying the Main Range, in most cases, do not have the character of continuous chains, but are short ridges or mountain groups connected with the watershed ridge by spurs and cut through in many places by deep gorges of rivers, which, starting in the Main Range and breaking through the advanced heights, descend to the foothills and out onto the plains.

Thus, almost along its entire length (to the west from the south, to the east from the north) a number of high basins adjoin the watershed ridge, in most cases of lacustrine origin, closed on the one hand by the heights of the watershed, as well as its spurs, and on the other by separate groups and short ridges of advanced hills, which in some places surpass the main chain in height.

On the north side of the watershed, transverse basins predominate, and on the south, except for its western extremity, longitudinal ones. It is also characteristic of the Caucasus Range that many of the primary peaks do not lie on the watershed ridge, but on the extremities of its short spurs heading to the N (this is the position of the peaks: Elbrus, Koshtan-tau, Adai-khokh, etc.).

The northern, more developed slope of the Caucasus Range, formed by many spurs, adjoining in general almost perpendicular to the Main Range and separated by deep transverse valleys, reaches a very significant development in the vicinity of Elbrus (Elbrus ledge). The most significant uplift is directed from this peak directly to the north, serves as a watershed between the waters of the Kuban and the Terek, and, descending further in ledges, spreads into the vast Stavropol Upland (see the Caucasian Territory).

The northern slope is even more developed in the eastern part of the Caucasus Range, where numerous, and very significant in height and length, its spurs form the vast mountainous country of Dagestan (Dagestan ledge). Gradually lowering to the north, the northern slope is formed by many advanced hills, which in places are in the form of ridges; these include the so-called Black Mountains, running north of the Main Range at a distance of 17-60 century. To the north, the Black Mountains form gentle and long slopes, in most areas covered with dense forests (hence the name), and to the south they fall in steep cliffs. The rivers flowing from the Main Range break through the Black Mountains along deep and narrow, very picturesque gorges; the height of this advanced chain is, in general, insignificant, although in the upper reaches of the Ardon and Urukh some of their peaks reach more than 11 tons. high (Kion-hoh 11230 ft., Kargu-hoh 11164 ft.).

The southern slope is especially poorly developed in the western and eastern parts of the ridge, reaching a rather significant orographic development in the middle, where it is adjoined by parallel hills that form longitudinal valleys of the upper reaches of the Rion, Ingur and Tskhenis-tskhali, and long spurs extend to the south, separating the Alazani basins. , Yora and Kura.

This slope is distinguished by remarkable steepness and low development where it falls to the Alazani valley; Zagatala, located at an altitude of 1783 feet. at the southern the soles of the Caucasus Range, is separated in a straight line by only the 18th century. from its crest, reaching here more than 11,000 ft. heights above sea level. The Caucasian ridge is not distinguished by cross-country ability; only for app. and east. its extremities have convenient and low passes, quite accessible all year round for communication.

Throughout the rest of its length, with the exception of the Mamison and Krestovaya (see Georgian Military Road), the paths through the ridge in most cases represent pack or even hiking paths, partly completely inaccessible for use in the winter season. From all the passes highest value has a Cross (7977 ft.), through which the most significant traffic is carried out along the Georgian Military Highway throughout the ridge.

seven parts

For a more convenient view, the Caucasus Range can be divided along the length from W to E into seven parts: 1) the Black Sea Caucasus (from the meridian of Anapa to the Oshten mountain group - about 250 in.), 2) the Kuban Caucasus (from Oshten to the source of the Kuban - 150 c.), 3) the Elbrus Caucasus (from the source of the Kuban to the top of Adai-khokh - 160 c.), 4) the Terek Caucasus (from Adai-khokh to the city of Barbalo - 120 c.), 5) the Dagestan Caucasus (from Barbalo to peaks of Sari-Dag - 140 c.), 6) the Samur Caucasus (from Sari-Dag to the city of Baba-Dag - c. 120 c.) and 7) the Caspian Caucasus (from Baba-Dag to the top of Ilkhi-Dag - about 160 in.).

Black Sea Caucasus

The Black Sea Caucasus along its entire length runs almost parallel to the Black Sea coast, and the distance of the watershed ridge from the sea does not exceed 40 century. (at Oshten); not reaching the snow line anywhere, the Black Sea Caucasus rises here and there to 6 t. ft. only in the southern part; between the passes are remarkable Novorossiysk - 1225 ft. and Goythsky - 1343 ft. (between Tuapse and Maykop), designed for wheeled traffic.

Cool south. the slope falling to the Black Sea is divided by short buttresses of the ridge into a series of transverse valleys and gorges, along which rivers flow into the sea.

The northern, much more developed slope is formed by spurs gradually lowering towards the Kuban plane, between which there are lion valleys. tributaries of the Kuban (Psekups, Pshish) and Belaya (Pshekha) rivers.

Kuban Caucasus

The Kuban Caucasus begins with the Oshten mountain group (the top of Fisht - 9360 ft. above sea level), on the top of which eternal snow appears for the first time, differs, in comparison with the Black Sea, in greater height and width, in snow covering its most prominent peaks, a significant height and the difficulty of the passes, and, finally, the appearance of glaciers, which are first encountered in the upper reaches of the Laba; at the same time, the height of the watershed ridge gradually increases from NE to SW.

Of the peaks, except for Fishta, the following are remarkable: Shugus (10642) and Psysh (12427). Of the passes that rise very significantly in this part of the ridge and represent pack trails, Pseashkho is remarkable - 6870 feet. (from the Mzymta basin to the upper reaches of the Laba), Marukhsky - 11000 ft., Klukhorsky - 9075 ft. and Naharsky - 9617 ft. (the last two from the Kodor basin to the upper reaches of the Kuban).

The penultimate of the passes is the most convenient way of communication between Sukhum and Batalpashinsk. The southern slope of the Kuban Caucasus is more developed than in the previous part of the range; between its numerous spurs, descending to the Black Sea, lies a series of deep basins containing small river basins, the upper part of which is sometimes located almost parallel to the watershed ridge; such are the basins of Mzymta, Bzyb and Kodor. The northern slope is highly developed and has up to 100 e. in length; between its huge buttresses, of which the largest departs to the northwest from the top of Psysh, there are deep, wild and picturesque, forested transverse valleys and gorges of the upper reaches of the Kuban system (pp. Belaya, Laba, Urup, Zelenchuk, Teberda and Kuban); of these valleys, the valley of the upper Laba - Zagdan (see) is most famous.

Elbrus Caucasus

The Elbrus Caucasus, stretching from the origins of the Kuban to the top of the Adai-Khokh or to the upper reaches of the river. Ardona, represents the highest part of the Caucasus Range, rich in snow and glaciers. The average height of the Elbrus Caucasus reaches 11-12 t. ft.; passes that are difficult to access go down a little lower, but many times. its high peaks, bearing masses of snow and ice, rise above 16 t. ft.

From the Main Range to the NE, short and powerful spurs extend, in which the highest peaks of the Caucasus are located; in the most significant of these spurs, in the 20th century. north of the watershed ridge, rises Elbrus, or Mingi-tau (18470 ft.), the highest peak in the system of the Caucasus Range and within the Caucasus region. To the south of the Main Range, at a short distance, almost along the entire length of the Elbrus Caucasus, runs parallel to the Main Range, the Svaneti Range (top. Shoda 11128 ft.), Which, being approximately 3000 ft. on average, lower than the Main one, yet it goes far beyond the limits of eternal snow.

Between the Svaneti and watershed ridges there are high, parallel to the axis of uplift of the latter, the valleys of the Ingur and Tskhenis-tskhali, and the same valley of the upper reaches of the Rion adjoins the eastern tip of the Elbrus Caucasus from the south; these valleys, as well as the Ingura valley from the Kodor valley, are separated by high spurs of the Main Range. Between the peaks of the Elbrus Caucasus, in addition to Elbrus, there are remarkable: Dykh-tau (17054 ft.), Koshtan-tau (16881 ft.), Shkhara (17049 ft.), Dzhangi-tau (16564 ft.), Tetnuld (15914 ft.) , Ushba (15445 ft.), Adish (16291 ft.), Adai-hokh (15244 ft.), etc.

Through passes rising up to 12 tons. heights, partly over snow and glaciers, lead dangerous footpaths, along which the inhabitants of the upper reaches of the Rion, Ingur and Tskhenis-tskhali communicate with the northern slope. This latter, significantly developed in the western part, where the spurs of the Elbrus buttress slightly do not reach the line of the Vladikavkaz railway, is strongly shortened to the SE, as it approaches the top of Adai-hokh, where it is three times shorter than in the west. All spurs and buttresses of the northern slope are directed to the NE and between us, in deep gorges and valleys, the rivers of the Terek system (Baksan, Chegem, Cherek, Urukh) flow in the same direction, originating in the vast glaciers of the Caucasus Range.

Terek Caucasus

The Terek Caucasus, embracing a part of the ridge from Adai-khokh to Mount Barbalo (10807 ft.), is characterized by many features. The entire Caucasian ridge narrows strongly here, its slopes, and especially the northern one, become short and, in addition, the watershed ridge, deviating here in the upper reaches of the Terek and Ardon to the south, is significantly inferior in height to the front ridge located somewhat north of it, with its peaks almost reaching the heights of the Elbrus Caucasus and, in essence, being, as it were, a direct continuation of the latter. The main peaks of the watershed ridge, except for Barbalo: Zilga-hokh (12645 ft.), Zikari (12563 ft.), Choukhi (12107 ft.), while in the advanced: Tepli (14510 ft.), Dzhimarai-hokh (15673 ft. .), Tsmiakom-khokh (13567 ft.) and, finally, Kazbek (16546 ft.). Between the passes in this part of the Caucasus Range, which drops significantly towards B, are remarkable: Mamisonsky (9390 ft.), Through which the Ossetian Military Road passes, connecting Kutaisi with Vladikavkaz; Roki (9870 ft.) - Leading from the Ardon basin to the Great Liakhvi basin, and in particular the Cross (7977 ft.), through which the Georgian Military Highway is laid.

The amount of glaciers and snow in the Terek Caucasus, although less than in Elbrus, is still very significant. Four high, separated from one another by high spurs, transverse basins adjoin the watershed ridge in the Terek Caucasus: Ardonskaya, Terskaya, Assinskaya and Argunskaya, in which, partly from glaciers, the rivers of the Terek system originate: From the rivers that arise in them, Ardon and Terek break through to the N through the front ridge along grandiose gorges, of which the Darial gorge is especially remarkable, through which the Terek flows. To the east of the Georgian Military Highway, the northern slope of the Caucasus Range again becomes more extensive, reaching a very significant development on the Barbalo meridian. The southern slope of the Terek Caucasus is more developed than in other parts of the Caucasus Range; it is formed by many long low spurs and buttresses gradually descending to the south, some of which go to join the Lesser Caucasus (the Suram Range from the top of Zikari), while others go far to the southeast, separating the valleys of Iora and Alazani and merging with the steppes of the east. Transcaucasia to the SE from Tiflis. From the southern slope of the Terek Caucasus flow: Iori, Bolshaya Liakhvi, Aragvi and other left tributaries of the Kura, forming deep transverse valleys in their upper reaches.

Dagestan Caucasus

Dagestan Caucasus, stretching from the city of Barbalo to the top. Sari-Dag (12008 f.), is characterized by an unusually complexly developed northern slope, which is composed of many high and long spurs extending from the Main Range to the NE and forming a mountainous country - Dagestan, and a remarkably short, steep and undeveloped southern slope, which, however, retains , the same character and further to the SE in the Samur and Caspian Caucasus, the height of the watershed ridge of the Caucasian ridge in the Dagestan Caucasus is lower than in the Terek, and it represents few peaks protruding above the ridge; glaciers and eternal snows are present on it only in a small amount. Powerful sowing is much higher and more abundant with glaciers and snow. spurs and advanced chains of the K. ridge that fill Dagestan. The most app. the spur is the Sulako-Tersky (Perikitelsky) ridge, which serves as a watershed between the Terek and Sulak, Bogossky, between the Andi and Avar Koisu and Naukat, separating the last river from the Kara-Koisu.

Narrow and deep transverse valleys closed by the indicated spurs adjoin the watershed ridge of the Caucasus Range in the N: Tushinskaya, Didoyskaya and Ankratlskaya. In the first two, the Andean Koisu originates, and in the last, the Avar, breaking through the advanced heights of the Caucasus Range and carrying their waters to the N - to Sulak. The same character has pp. Kazikumukhskoye and Kara-Koysu, flowing down from the north. the slope of the spur separating the basins of the Samur and Sulak and heading to the E from the top. Sari-dag. A collection of high ridges, with innumerable spurs and buttresses, forming in some places vast plateaus, mostly rocky and devoid of forests, the predominance of broken lines and grayish-yellow colors in the landscape, deep gorges with fast-moving koisu (river), and poor communication lines - are features of Dagestan. More remarkable peaks, except for Barbado and Sari-dag: Ninikos-tsikhe (10251 ft.), Antsal (11742 ft.), Shavi-klde (11314 ft.) and others in the watershed ridge, Tebulos-mta (14781 ft.) , Donos-mta (13736 ft.), Big Kachu (14 0 27 ft.) in Sulako-Tersky and Balakuri (12323 ft.) in the Bogossky ridge. Between the passes, the most common are: Kodorsky (9300 ft.) and Satskhenissky, leading from Kakhetia to Dagestan. The southern short slope of the Caucasian Range falls steeply to the Alazani valley.

Samur Caucasus

The Samur Caucasus, stretching from Sari-Dag to Baba-Dag (11,934 ft.), is similar to Dagestan in the development of its slopes, but the height of the watershed ridge in it is greater than in the latter, and the amount of snow on the ridge again increases. Of the spurs, the one that goes from Sari-Dag to B and serves as a watershed between Sulak and Samur is remarkable, and from the advanced heights of Shah-Dag (13951 ft.), On which there are the last, towards E, eternal snows and glaciers of the Caucasus Range . Of the peaks of the watershed ridge, the following are remarkable: Gudur-dag (11075 ft.), Salavat-dag (11943 ft.), Thfan-dag (13764 ft.) and Bazar-duz, or Kichen-dag (14722 ft.). Passes: Gudursky (10118 ft.), leading from Zakatal to the upper reaches of the Samur, and Salavatsky (9283 ft.), along which the Military Akhta road runs. Sev. the slope of the Samur Caucasus, which by nature has much in common with Dagestan, of which it forms a part, belongs to the Samur basin, the upper part of which forms a vast longitudinal valley adjacent to the N to the watershed ridge. The southern slope falls to the Alazani valley and is partly irrigated by small steppe rivers flowing through the Nukhinsky district of the Elisavetpol province.

Caspian Caucasus

The Caspian Caucasus - the last link of the Caucasus Range - embraces it east. extremity from Baba-dag to Ilkhi-dag. Its highest points do not exceed 9000 feet. and completely devoid of snow cover. The Alty-Agach pass, on the road from Shamakhi to Quba, has no more than 4354 feet. height. The southern slope of the Caspian Caucasus is somewhat more developed than in the Samur and Dagestan, but even here it is inferior in this respect to the north; however, barely noticeable elevations are visible even at 40 ° N. sh., much south of Baku.

Snow

The height of the snow line on the Caucasus Range is not the same everywhere; depending on the climatic conditions, different for app. and eastern parts, as well as on the sowing. and southern slope of this mountain system, the position of the border of snows n. ur. m. varies greatly. The first snowy peak to the west is Oshten (Fishta), on which the line of perpetual snow is not higher than 9000 feet, and to the south. on a slope it drops even to 8900 ft.; further to B, under the influence of a decrease in precipitation and air humidity, the snow line gradually rises; on Elbrus, it is at an altitude of about 10,700 feet. (west and east slope) - 11700 ft. (northern slope). To the east of the meridian of Kazbek, due to a significant rise in the snow line and a decrease in the height of the ridge, only a few mountain peaks remain covered with eternal snow. Its limit at Shahdag is on average 12,200 feet. above sea level (northern slope 11900 ft., southern slope - 12500 ft.). Thus, the difference in snow height on the west. and east. extremities of the snowy region of the Caucasus Range reaches approximately 3200 ft. (on the south slope up to 3600 ft.). Snow on the north slope of the Caucasus Range, with a few exceptions, rise 1000-1500 ft. higher than to the south, which can be explained by the fact that sowing. the slope faces the dry open steppe spaces of Ciscaucasia. It is believed that out of the entire length of the watershed ridge, no more than 300 century BC are covered with eternal snow. In addition to the watershed ridge, there are significant masses of snow on the frontal ridges and ridges closest to it and the spurs extending from it (the front ridge in the Terek Caucasus, the Svanetsky ridge, the Sulako-Tersky, Bogossky, etc.).

Glaciers

The study of the glaciers of the Caucasus Range, which has moved far beyond recent times, far from finished; for many of them there is only scarce information, and the number of all glaciers, their distribution, area and other data are almost unknown. Nevertheless, it turned out that the previous opinion about the extremely insignificant glaciation of the Caucasus is incorrect and that in terms of the number of glaciers, their area and size, the K. ridge is almost as good as the Alps. The largest number of significant glaciers is located in the Elbrus and Terek parts of the ridge, and the number of glaciers of the 1st category in the basins of the Kuban, Terek, Liakhva, Rion and Ingur is determined, according to some data, at 183, and the 2nd category - at 679. The number of all glaciers in the Caucasus system , in all likelihood, at least 900-1000. The size of the Caucasian glaciers is very diverse and some of them (Bizingi) are not inferior in size to the Alech glacier (Alps). The Caucasian glaciers nowhere descend as low as, for example, the Alpine glaciers, and in this respect represent big variety; so the Karagom glacier releases with its lower end up to 5702 ft., and the Shah-Daga glacier up to 10374 ft. The most famous glaciers of the Caucasus Range are:

Name of the glacier	The mountain that descends	Height of the lower end of the glacier, in m	Glacier length, in km Total	Glacier length, km Without firn
Bizingi (bass. Cherek)	Shkhara, Dykh-tau	1993	19.6km	16.1km
Dykh-su	Shkhara, Dykh-tau	2027m	14.3km	10.1km
Karagom (bass Uruha)	Adai-hoh	1764m	15.5km	9.6km
Zanner (bass. Ingur)	Tetnuld	2084m	13.1km	10.0km
Devdoraksky (bass Terek)	Kazbek	2296m	5.7km	3.4km

During the Ice Age, the glaciers of the Caucasus Range were incomparably more numerous and extensive than they are today; from the numerous traces of their existence, found far from modern glaciers, it can be concluded that the ancient glaciers extended in length 50, 60 and even up to a hundred and more miles, descending into valleys up to 800-900 feet. above sea level. Currently, most of the glaciers of the Caucasus Range are in a period of retreat, which has been lasting for several decades.

Geology

Geologically, the Caucasus Range (according to Suess) represents two different parts: western and eastern; in the first of them, the crystalline base, on which the Jurassic, Cretaceous and Paleozoic deposits were located, is a fold overturned to the south, while in the second part the crystalline base has sunk and is hidden under the Kura lowland. On the southern slope east. parts of the Caucasus Range, a number of parallel discharges are observed, while in the sowing. Mesozoic and Miocene strata show folding, decreasing towards the north.

Crystalline schists and granites, of which the crest of the ridge to the west is composed, serve as the basis for the volcanic massifs of Elbrus and Kazbek, around which basalts, trachytes, and other igneous rocks are developed over a vast extent.

The Black Sea Caucasus is composed mainly of rocks of the Cretaceous and part of the Jurassic systems;

In Russia, there are regions with stunning mountain landscapes. The highest and most impressive peaks are located on the Main Caucasian Range. Throughout the mountain range, the peaks are distinguished by their height and massiveness. The direction of the ranges of the Caucasus Mountains is from northwest to southeast.

Caucasian region

Where do you think the Caucasus is located? This amazing mountainous area is located between the Black and Caspian Seas. It includes the mountains of the Greater and Lesser Caucasus. The Caucasus Range includes the Riono-Kura depression (depression), the coast of the two above seas, the Stavropol Upland, a small part of Dagestan, that is, the Caspian lowland, as well as part of the Kuban-Azov slopes.

The main peak of the ridge is the snow-white Mount Elbrus. The entire system of the Main Caucasian Range occupies approximately 2600 km². The northern slope covers about 1450 km², and the southern one - about 1150 km². Now let's take a closer look at the description of the mountain range.

Description of the Greater Caucasus Range

Fans of extreme sports, whether climbers or mountain skiers, have chosen this place for a long time. Those who traveled through the mountains of the Caucasus return to these places again. Thrill-seekers come here from all over the world for thrills.

The main Caucasian ridge, the photo of which is presented in the article, divides the Caucasus into two historical and cultural regions: Northern and Southern. You can find the ridge on the map between the Black and Caspian Seas. For convenient viewing, the mountain range is usually divided into 7 parts:

1. Black Sea Caucasus (from Anapa to Oshten - 265 km).
2. Kuban Caucasus (from Oshten to the source of the Kuban - 160 km).
3. Elbrus Caucasus (from the source of the Kuban to the peak of Adai-hokh - 170 km).
4. Terek Caucasus (from Adai-khokh to the city of Barbalo - 125 km).
5. Dagestan Caucasus (from Barbalo to the top of Sari-Dag - 130 km).
6. Samur Caucasus (from Sari-dag to the city of Baba-dag - 130 km).
7. Caspian Caucasus (from Baba-dag to the top of Ilkhi-dag - 170 km).

As you can see, 7 regions of the Greater Caucasus Range are divided into approximately equal sections in length.

The height of the mountains is varied: it ranges from 260 to 3360 meters. The climate in these places is light and mild, and in combination with beautiful landscapes, this corner of the planet becomes an ideal place for active rest winter and summer.

The Caucasian Range is mainly composed of limestone. In ancient times, this place was located on the ocean floor. Today, if you look at the mountain range from a bird's eye view, you can see the folds of mountains, a huge number of glaciers, active rivers and deep lakes. High basins can be observed along the entire length of the mountain range.

A few words about the northern slope

This side of the Main Caucasian Range is well developed. It is formed from a large number of spurs that adjoin at an angle of 90̊ to the main ridge. The Elbrus fault zone separates the waters of the Caspian Sea and the Kuban. Further, this section decreases in ledges and gently passes into the mountains of Pyatigorsk, as well as the Stavropol Upland.

More developed mountains are located on the northern slope of the Caucasus mountain range on the eastern side, where Dagestan is located. Heading north, they decrease, from there the mountain ranges called the Black Mountains begin. They are gentle and long slopes. Why do you think they were called Black? The thing is that their slopes are covered with dense and impenetrable forests. The height of the Black Mountains is insignificant. However, there are peaks in this area, the height of which reaches 3500 meters. Such peaks include Kargu-Khokh, Vaza-Khokh and others.

Information about the southern slope

Compared to the northern slope, the southern one is much less developed, especially the eastern and western parts of the Caucasus Range. Looking at the map, you can read that this section of the mountain range is adjoined by hills that form the longitudinal valleys of the Enguri, Rioni, and Tskhenis-Tskhali. To the south of the mountain range there are very long spurs that separate the basins of the Alazani, Kura and Iori rivers.

The steepest section of the southern side of the ridge is Mount Zagatala. Its height reaches 3 km above sea level.

Otherwise, the Main Caucasian Range from the south side is passable, with the exception of two passes: Cross and Mamison. Roads across the range are accessible almost all year round. In some places they resemble pack trails.

The Cross Pass is of great importance in this area, as the Georgian military road passes through it.

About glaciers

Few people suspect, but the size, number and area of ​​​​the glaciers of the Caucasus Range, the photo of which is given in the article, are practically not inferior to the glaciers of the Alpine Mountains. Them largest number concentrated in the region of the Elbrus and Terek ridges.

There are about 183 glaciers of the first order in the basins of the Kuban, Rioni, Terek and Inguri rivers. And there are several times more glaciers of the 2nd category - about 680. Soviet years large studies were carried out in the Caucasus, as a result of which geologists compiled the Catalog of Glaciers of the USSR. Soviet scientists in the early 80s counted 2050 glaciers. Their total area was almost 1500 km2.

As for the glacial dimensions of the Caucasus Range, there is no unequivocal answer. Their area is varied. For example, the Bezengi glacier is almost as large as the Alechsky glacier, which is located in the Alps. The Caucasian masses of ice, unlike the Alpine ones, never descended low. The most famous are the Bezengi, Chatyntau, Tsey, Big Azau and Tsaneri glaciers. Bezengi is the largest glacier in the Caucasus Range. Its length is 17 km.

During the Ice Age, the ice masses of the range were larger and more numerous than they are today. In our time, they are in the stage of retreat, which has been going on for more than a dozen years.

Bezengi

This is a mountainous region located in Kabardino-Balkaria. It is considered the central range, as well as one of the highest parts of the Caucasian chain. It includes the Bezengi wall. It is a 42-kilometer array of mountains. This is a high section of the ridge. The borders of the Bezengi Wall are considered from the west - the peak of Lyalver, and from the east - Mount Shkhara.

From the north, the Bezengi wall abruptly breaks up to 3 thousand meters in the direction of the Bezengi glacier. In Kabardino-Balkaria it is also called Ullu-Chiran. On the Georgian side, the relief is complex, there is even a glacial plateau. The most significant peaks of the region are the Bezengi Wall, Yesenin Peak, Shota Rustaveli Peak, Lyalver, Dzhangitau and others.

The main peak of Georgia

The highest point in Georgia is Shkhara Peak. Its height above sea level is 5193 meters, but some researchers claim that it is higher - 5203 m. The mountain peak is located about 90 km north of the city of Kutaisi. Shkhara is the third highest peak in the Caucasus and Russia.

The mountain is composed of schist and granite. Its slopes are covered with snow-white glaciers: on the north side - the Bezengi glacier, and on the south - Shkhara. This place is popular among climbers. The first ascent of this mountain was made in 1933. The hill is also notable for the fact that on the side of the southern slope at an altitude of 2000 meters there is a village that is included in the UNESCO list.

Tsey glacier

And now let's talk about the glacier, which is located in the North Caucasus. The Tsey glacier is one of the largest and lowest descending glaciers in the Caucasus. You can find it in North Ossetia. It feeds on snow from the top of Adai-Khokh. The height of the glacier is about 4500 meters. It descends to a height of 2200 m above sea level. Firn fields, consisting of grain snow, reach about 9 km. Below the glacier is narrow, and the higher it is located, the more it expands. It is constrained by rocks, so it is dotted with cracks, and there are also icefalls.

The Tsey glacier consists of large and small branches. There are four in total. There is also a river that flows out of a beautiful ice arch. Its channel passes through picturesque places rich in century-old pines. Nearby there is a camp site "Ossetia", climbing camps, hotels, a weather station and the Caucasian Mining and Metallurgical Institute. Two cable cars are laid to the glacier. Yuri Vizbor wrote poems about this beautiful place. The local peoples composed legends, songs and tales a lot about the glacier.

Mount Achishkho

This mountain range is located on the side of the western Caucasus. Belongs to the Krasnodar Territory. The height of the mountain reaches 2400 meters and is located 10 kilometers from Krasnaya Polyana. This ridge differs from all others in its rock composition. It consists of shale and volcanic rocks. The landscapes have ancient glacial landforms, karst lakes and even waterfalls. The mountains are surrounded by a humid climate, with up to 3 meters of precipitation per year. It is considered the largest value in Russia. The snow cover is about 10 meters. As you may have guessed sunny days in a year in this mountainous corner is very small - no more than 70 days.

The slopes of Mount Achishkho on the north side are covered with fir forests. Mountain meadows are located on the peaks, broad-leaved and beech forests grow on the other sides. This place is popular among hikers. Here you can find dolmens - stone buildings of ancient peoples.

biosphere reserve

On the territory of the Western Caucasus there is a reserve, its total area reaches about 300 thousand hectares. In February 1979, the UNESCO organization decided to assign biosphere status to the reserve.

In 2008, he was named after Kh. G. Shaposhnikov, the founder of the Caucasian Reserve. But he became famous not only for this, but also for his perfect discoveries in the field of biology. At the beginning of the 20th century, the scientist noticed that the Caucasian bison was disappearing in this area, so in 1909 he wrote a letter to the Russian Academy of Sciences with a request to equip the reserve. But since the land belonged to the Kuban Cossacks, things did not move forward for a very long time. The scientist made several attempts, and 10 years later, namely in 1919, things got off the ground. In 1924, the bison reserve began to function.

Conclusion

We have traveled from the foot of the Black Sea Mountains to the Caspian peaks. Thus, the length of the Caucasus Range is 1150 km. Now you know that it is divided into Northern and Southern historical and cultural regions. The total length of the ridge is divided into 7 parts, each of which has almost the same length. Each mountain region is characterized in its own way.

Those who are planning to make a trip should definitely visit the Caucasus Mountains. You will remember these fabulous landscapes for a lifetime. Terrenkur, rock climbing, river rafting, skiing and many other outdoor activities offer tourists the Caucasus.

General character of the Caucasus Mountains. - Snow-covered parts of the Main Range. - The main ridge between Elbrus and the Georgian military road. - The eastern part of the Main Range between Begyul and Baba-dag. - Part of the Main Range, lying to the west of Elbrus and up to Mount Oshten. - The total length of the part of the Main Range covered with eternal snow. - Lateral ridge. - The highest points of the eastern part of it. - Pirikiteli and Bogosskiy ridges. - Western part of the Side Range. - Ararat, Alagyoz and other high points of Transcaucasia.

The high Caucasian ridge with its countless spurs and gorges is a gigantic threshold rising between Europe and Asia. Not only in its geographical position, but also in many other respects, it represents an intermediate or transitional link between the mountains of the two parts of the world mentioned. This is the first mountainous country from Asia, says K. Ritter, which is distinguished by European construction. Like the European Alps, it narrows in the west and widens greatly in the east, reaching nearly 50 geographical miles of width near the shores of the Caspian Sea. The northwestern part of the Caucasus, with its abundance of forests, resembles the mountains of Europe, while the southeastern part (Dagestan, in particular) approaches the mountains of Central Asia with its bare, lifeless cliffs.

“Here, on the threshold of Europe,” says Ritter, “begins the characteristic form of tall trees, which is the distinctive character of Central Europe. German oak (Quercus robur) and German beech (Fagus silvatica) overshadow the dwellings of the Indo-Germanic tribes in the North Caucasus.”

In terms of the height of the snow line, in terms of the size of both modern glaciers and glaciers of bygone eras, the Caucasus, as we will see below, also occupies the middle between the mountains of Europe and the giant ridges of Central Asia. Finally, by the height of the primary peaks, the average height of its crest, and some other features, the Caucasus also represents an intermediate link between the extreme members mentioned.

The well-known Russian scientist and traveler I. V. Mushketov says that, while doing research in Central Asia, he more than once came across questions that are completely insoluble with the help of those doctrines that were developed during the study of Europe, and that the study of such an intermediate area, like the Caucasus, should shed light on the study of Asia. Here, therefore, in particular, that fruitful idea is expressed, which was developed by Ritter in his numerous writings, namely, that Earth is not a lifeless mass, but an organism, all parts of which are in close connection and strict dependence on each other.

From the foregoing, the reader will understand that it is impossible to study the Caucasus, completely isolating it from the other mountains of both Europe and Asia, and that I will, of necessity, have to touch the mountains and glaciers of other countries from time to time, although in general terms.

The main Caucasian ridge is a continuous chain of mountains stretching from the Black Sea to the Caspian Sea for 1420 versts. The highest part of it lies between Elbrus and Kazbek, and especially between Elbrus and Adai-khokh. Between the last two points, as E. Favre notes, there is not a single pass below 3 thousand meters (9840 feet) above sea level. To the east of Adai-hoch, which has 15,244 lbs. (4647 m) of height, the Main Range drops strongly, forming the so-called Mamissonovsky Pass (9300 ft., or, according to Favre, 2862 m). Still further to the east it rises again, with some peaks exceeding 12,000 feet. (Zekari and Zilga-hoch reach over 12,500 feet in height); further east again follows a decrease. Here is the Buslachirsky pass (7746 f.) between the Terek and Aragva and the pass of the Georgian Military Road, or Krestovy (7957 f.), behind which the Main Range in a distant space (300 versts) is almost devoid of snow and ice. Finally, in the eastern part, in an area of ​​80 versts, precisely between Begyul and Baba Dag, it again rises strongly, reaching an average height of 12,664 feet, while individual points of it rise still much higher. Behind Baba-dag, having 11,934 l. height and separated only by 70 versts in a straight line from the Caspian Sea, the mountains gradually lower and, finally, merge with the low-lying seashore.

To the west of Elbrus, the ridge also drops, but here the snow line also drops very noticeably, so that, starting from Elbrus and up to the upper reaches of the Bolshaya Laba on the north side and the Bzyb on the south, the peaks of the Main Range rise significantly above the snow line and therefore are covered with almost continuous eternal snow. Mount Psysh, whose snows nourish both Laba and Bolshoy Zelenchuk, is the extreme point in the west, exceeding 12,000 pounds. height. Beyond Psysh, the mountains, descending more and more, reach Oshten and Fisht, which make up one mountain range, rising to 9369 feet. (2856 m). This is the most extreme point in the west of the Main Caucasian Range, where you can still find eternal snow. Between Oshten and Psysh, the ridge is covered with snow, but not everywhere, but only in higher places. Further to the east, snow is visible on Abago and Shugus (10,624 ft.).

To the west of Oshten, the mountains immediately drop sharply, their crest is almost devoid of high bare rocks and is covered not only with meadows, but even with forests. It retains a similar character to the very shores of the Black Sea.

Thus, except for several peaks located in the eastern half of the Main Caucasian Range, only that part of it, which lies between the upper reaches of the Bolshaya Laba and the Georgian Military Highway, has the conditions necessary for the development of glaciers. This part, however, represents almost one-fifth of the entire Main Range. It is only about three hundred versts long, except for all the meanders.

The distribution of glaciers and eternal snows in the Caucasus is not limited, however, to the Main Range. The Caucasus, as noted by the famous geographer Karl Ritter, is similar in its relief to other ranges of Europe and is very different from the mountains of Asia. It is in it that there are nowhere such high plateaus that distinguish the mountains of Asia, but it represents a very complex system of high mountain ranges and their spurs. Thus, almost in the very middle of the Main Range, exactly where Adai-khokh rises, the Side Range intersects with the Main Range. To the west of Adai-khokh, this ridge stretches along the southern side of the Main, is separated from it by an average number of 25 versts, and reaches the Black Sea near Gagra. The other part of the Side Range, namely the one that stretches east of Adai-khokh, passes to the northern side of the Main Range, runs almost parallel to it, on average 20 versts from it and reaches the Caspian Sea.

The main Caucasian ridge, along its entire length from the Black to the Caspian Sea, is nowhere interrupted by transverse valleys and gorges, and represents a real watershed line, taken as the border between Europe and Asia; The side, of course, cannot form such a continuous ridge as the main one. Its western part is interrupted by the following rivers: Rion, Tskhenistskhali, Ingur, Kodor and Bzybyu, and the eastern part - by Ardon, Terek, Argun, Andi Koisu, Avar Koisu and Samur.

Some parts of this ridge far exceed the parts of the Main one lying next to them, and in the same way, individual peaks of the first ridge rise above the highest (with the exception of perhaps 3-4, which are: Elbrus, Dykh-tau, etc.) points of the second. It is even possible that the highest part of the Lateral Range, lying between Adai-khokh and Kazbek, exceeds the highest part of the Main Range. In addition, most of the highest points of the Caucasus lie in this side chain. They include: Kazbek 16 546 f. (5043 m), Dzhimarai-khokh 15,694 f. (4783 m), Syrkhu-Barzoy 13,637 f. (4153 m), Tepli 14,510 f. (4422 m); and even further to the east, namely near the headwaters of the Argun, Avar and Andi Koisu, the side chain forms two very high ridges located north of the Main one, and has the following very high points: in the Pirikite ridge - Tebulosmta 14,781 f. (4506 m), Small Kachu, Diklosmta 13,717 f., Big Kachu 14,027 f. (4276 m), Kvavlosmta 13 7002, and in Bogossky - Ballakuri 12 323 f., Bochek, Kavalavissa and others. In addition, the peaks of the easternmost part of the Caucasus, namely: Shah-Dag (13,951 lbs.), Shalbuz-Dag (13,679 lbs.), Kizilkaya (12,247 lbs.), Are included in the Lateral Range.

The western part of the Side Range is much lower than the eastern part, and is completely devoid of particularly high peaks. Among the most exalted belongs Shoda (on the five-verst map of the Caucasus - Shoba), located on the right side of Rion, not far from Oni, and reaching 11,128 f. On top of it lies several snow fields. To the west of Shoda stretches the Svaneti Range; in the space of 20 versts, namely, almost from Mushur to Lyaila, it is covered with snow. The peaks of Lakura, Lyaila and Lyasil, as well as many other sharp teeth of this ridge, rise far above the snow line. To the east of Mushur, eternal snows are on Dadiash 5. According to Ilyin, the Svaneti Range is not inferior in height to that part of the Main Range that limits Svanetia from the north, and extends between Uzhba and Tetnuld, these paramount giants of the Caucasus Range. Many glaciers also descend from the northern slope of the Svaneti Range, and the southern one is dotted with snow spots. However, it should be noted that due to the proximity of the Black Sea and the abundance of precipitation, the snow line here lies lower than on most of the Main Range.

Even further to the west, that is, on the mountains located between Ingur and Kodor, there are probably also peaks covered with snow, but this area is very little known. The snowy peaks in both parts of the Side Range occupy a total of 273 versts in length, and together - the Side and Main Ranges - about 570 versts. Thus, only for 570 versts the mountains of the Greater Caucasus are covered with snow and glaciers.

This account does not include, however, those few points in the South Caucasus that rise above the snow line. These include: Big Ararat (16,916 lbs., 5160 m) and Alagoz (13,436 lbs.). In addition, in the eastern part of the Pontic Range, which runs along the southern coast of the Black Sea, there are also a few peaks that rise to the line of eternal snows. Of these, Varchembek-dag, having 12,152 f. height and, according to Palgreve, strikingly reminiscent of the Matterhorn in its shape, is located within Turkey, and Karchkhal, towering in the Karchkhal ridge (a continuation of the Pontic), has 11,248 f. and is located within Russia (20 versts from Artvin. On all these peaks of the South Caucasus, with the exception of Ararat and Alagyoz, snow forms only small fields and narrow ribbons in summer that cannot give rise to glaciers. According to Masalsky, about the snow line on Pontisky the ridge is out of the question, and eternal snow is here only on Karchkhala.

In the southeastern part of the Caucasus, not far from the Persian border, there are also peaks that are freed from snow in rare years. To them belong: Kapujih, having 12,855 f. height and located 40 versts east of Nakhichevan, and Kazangyol-dag, rising to 12,649 ft. Small deposits of snow still remain southern slopes Gyamisha (l2,269), Ginal-dag (l11,057), and Murov-dag (l11,219); their northern side, which is under the influence of the sultry Elisavetopol valley, is freed from snow in the summer. Occasionally snow remains for a whole year on Godorebi (10,466 lbs.) and Abul (10,826 lbs.), towering on a ridge running along the border of Tiflis and Akhaltsikhe counties

Let us also mention two very high extinct volcanoes, although they do not belong to the Caucasus, but are located very close to it and not far from the shores of the Caspian Sea. One of them is called Damavend, and the other is Savalan. The first has £18,600 and the second £15,792. absolute height. Therefore, both of them rise above the snow line. On the northern slope of Damavend, which is influenced by the Caspian Sea, there is a lot of snow, there are even glaciers; Savalan has on its top, where in former times there was a crater, a lake with warm water. Probably, the excess of heat inside the mountain largely prevents the accumulation of snow on its slopes.

The Caucasus Mountains, as if holding together the space between the Black and Caspian Seas, consist of two mountain systems - the Greater Caucasus and the Lesser Caucasus. The Greater Caucasus is picturesque, majestic and famous. This is where everything starts major rivers region. Passes through it state border Russia with two states at once - Georgia and Azerbaijan.

From northwest to southeast, the Greater Caucasus lies almost 1150 km: near the Black Sea, its foothills rise in the Anapa region, and on the opposite side it begins at the Absheron Peninsula, not far from the capital of Azerbaijan. Near Novorossiysk, the width of this mountain system is only 32 km, near Elbrus, the Greater Caucasus is almost 6 times wider.

For ease of designation of peaks, this mountain range is traditionally divided by scientists into three sections:

The Western Caucasus (from the Black Sea coast to the foot of Elbrus) consists mainly of low mountains (up to 4000 m), the highest point is Mount Dombay-Ulgen (4046 m);

The Central Caucasus (Elbrus and the mountain range from it up to Mount Kazbek) has 15 highest peaks (5000-5500 m);

Eastern Caucasus (from Kazbek to the Caspian coast). The highest mountain in this part of the massif is Mount Tebulsomta (4493 m).

In addition, the Greater Caucasus is conditionally divided into three belts (longitudinal segments):

The axial part of the mountain system. It is based on the Main Caucasian (Vodorazdelny) ridge and next (on the left) - the Side ridge.

The northern slope belt is mainly parallel mountain ranges in the central and western parts of the Greater Caucasus. These ridges decrease to the north.

Southern slope of the mountain system. It consists mostly of echelon-shaped ridges that adjoin the GKH.

On the slopes of the Greater Caucasus lies a huge number of glaciers - more than two thousand. The glaciation area is approximately 1400 km². The largest glacier in the Greater Caucasus is Bezengi, its length is 17 km, it is located on the Bezengi wall. The record holder for the number of glaciers in the entire mountain system is Mount Elbrus. Most of all eternal ice located in the central part of the Greater Caucasus, about 70% of all glaciers are concentrated here. Thanks to a clear structure and white peaks, the mountains of the Greater Caucasus are clearly visible on the map, this mountain range cannot be confused with any other.

The main peaks of the Greater Caucasus

Elbrus is the highest point not only in the Greater Caucasus, but throughout Russia. Its height is 5,642 m. Elbrus is located on the border of Karachay-Cherkessia and Kabardino-Balkaria, it is the Mecca of mountaineering. Several of the highest climbing shelters in Europe have been built on its slopes.

Dykhtau (5204.7 m) is the second highest mountain in the Greater Caucasus, which is part of the Bezengi wall. Like Elbrus, Dykhtau is a “two-headed” mountain. The following in the list of the highest mountains of the mountain system - Koshtantau (5152 m) and Pushkin Peak (5100 m) - are also located in the massif of the Bezengi wall.

Dzhangitau (5085 m) is the central mountain of the Bezengi wall, a popular place for mountaineering. Located on the border of Russia and Georgia.

How did the Greater Caucasus appear?

A huge mountain system cannot have a simple geological structure. The tectonic structure of the Greater Caucasus is complex and heterogeneous, which is associated with the history of the formation of the mountain range. According to recent studies, the Greater Caucasus arose as a result of the interaction of the East European and Arabian lithospheric plates. Millions of years ago, this place was the bay of the ancient ocean Tethys, which united the Caspian, Black and Sea of ​​Azov. At the bottom of this ocean, active volcanic activity was going on, red-hot rock poured into the earth's crust. Gradually, mountain-like massifs were formed, which then went under water, then again rose on it, and as a result, in the middle of the Mesozoic, in those areas that became islands, sandy-argillaceous sediments were deposited, in some troughs these deposits reached several kilometers. Gradually, several islands formed one large island, which was located where the central part of the Greater Caucasus lies today.

At the beginning of the Quaternary period, the Arabian plate increased pressure on the East European one, the volcanoes Elbrus and Kazbek erupted - in general, the formation of the mountain range was active. The sediments on the slopes of the stone islands were compressed into complex folds, which were then subjected to faults. The central part of the modern Greater Caucasus has risen. Rock rose everywhere and unevenly, river valleys formed in the faults. At the same time, while the mountains were growing, their icing began against the background of a general cooling. The mountains were almost completely covered with ice. The movements of ice masses and frosty weathering completed the appearance of the modern mountains of the Caucasus: it was thanks to them that the relief form of the Greater Caucasus remained the way we know it now - with sharp ridges and moraine ridges.

The Greater Caucasus has long turned from a series of impregnable mountain walls into a territory completely inhabited by man. In river valleys, as well as on the slopes of mountains (sometimes quite high!) People live. There is a huge number of historical monuments dear to the people living here. Through the numerous passes of the Greater Caucasus, communication has been established between the republics within the Russian Federation, as well as with neighboring states.

The Caucasus Mountains are a mountain system between the Black and Caspian Seas. It is divided into two mountain systems: the Greater Caucasus and the Lesser Caucasus.

The Greater Caucasus stretches for more than 1100 km from the northwest to the southeast, from the Anapa region and the Taman Peninsula to the Absheron Peninsula on the Caspian coast, near Baku. The Greater Caucasus reaches its maximum width in the Elbrus region (up to 180 km). In the axial part there is the Main Caucasian (or Dividing) Range, to the north of which a number of parallel ranges (mountain ranges) extend, including a monoclinal (kuest) character. 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).

The Greater Caucasus is a region with a large modern glaciation. The total number of glaciers is about 2,050, and their area is approximately 1,400 km². 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). Major centers of glaciation are Mount Elbrus and the Bezengi wall. The largest glacier in the Greater Caucasus is the Bezengi glacier (about 17 km long).

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 largest lake is Sevan.

The Western Caucasus is a part of the mountain system of the Greater Caucasus, located to the west of the meridional line passing through Mount Elbrus. The part of the Western Caucasus from Anapa to Mount Fisht is characterized by low-mountain and mid-mountain relief (the so-called North-Western Caucasus), further east to Elbrus, the mountain system acquires a typical alpine appearance with numerous glaciers and high-mountain landforms. In a narrower sense, which is followed in mountaineering and tourism literature, only part of the Main Caucasian Range from Mount Fisht to Elbrus is referred to the Western Caucasus. On the territory of the Western Caucasus - the Caucasian Reserve, the Bolshoy Thach Natural Park, the natural monument "Buyny Ridge", the natural monument "Upstream of the Tsitsa River", the natural monument "Upstream of the Pshekha and Pshekhashkha Rivers", which are under the protection of UNESCO as a World Heritage Site. For climbers and tourists the most popular areas are: Dombay, Arkhyz, Uzunkol

Central Caucasus

The Central Caucasus rises between the peaks of Elbrus and Kazbek and is the highest and most attractive part of the entire Caucasus Range. All five-thousanders are located here along with their numerous glaciers, including one of the largest - the Bezengi glacier - 12.8 kilometers long. The most popular peaks are located in the Elbrus region (Ushba, Shkhelda, Chatyn-tau, Donguz-Orun, Nakra, etc.). The famous Bezengi wall with majestic surroundings (Koshtantau, Shkhara, Dzhangi-tau, Dykh-tau, etc.) is also located here. The most famous walls in the system of the Caucasus mountains are located here.

Eastern Caucasus

The Eastern Caucasus stretches for 500 km to the east from Kazbek to the Caspian Sea. It stands out: the Azerbaijan mountains, the Dagestan mountains, the Chechen-Tushet mountains and the Ingushet-Khevsuret mountains. Especially popular is the Erydag massif (3925m), located in the Dagestan mountains.

Being the border between Europe and Asia, the Caucasus has a unique culture. A large variety of languages ​​is concentrated in a relatively small area. The Caucasus and the ranges adjacent to it from the north and south were in ancient times the crossroads of great civilizations. Plots related to the Caucasus occupy a significant place in Greek mythology (myths about Prometheus, the Amazons, etc.), the Bible also mentions the Caucasus as a place of salvation of mankind from the flood (in particular, Mount Ararat). The peoples who founded such civilizations as Urartu, Sumer and the Hittite state are considered by many as people from the Caucasus.

However, the image of the Caucasus Mountains and the mythical and legendary ideas associated with them received the most complete display among the Persians (Iranians). Iranian nomads brought with them a new religion - Zoroastrianism and a special worldview associated with it. Zoroastrianism has had a serious impact on world religions - Christianity, Islam, and partly Buddhism. Iranian names have been preserved, for example, by the mountains and rivers of the Caucasus (Aba River - "water", Mount Elbrus - "iron"). You can also point to the particle “stan”, popular in the East, in such country names as Dagestan, Hayastan, Pakistan, which is also of Iranian origin and translates roughly as “country”.
The word "Caucasus" is also of Iranian origin, which was assigned to mountain ranges in honor of the epic king of Ancient Iran, Kavi-Kaus.

Approximately 50 peoples live in the Caucasus, which are designated as Caucasian peoples (for example: Circassians, Chechens), Russians, etc., speaking Caucasian, Indo-European, and also Altaic languages. Ethnographically and linguistically, the Caucasian region can be attributed to the most interesting areas of the world. At the same time, populated areas are often not clearly separated from each other, which is partly the cause of tensions and military conflicts (for example, Nagorno-Karabakh). The picture changed significantly, primarily in the 20th century (Armenian genocide under Turkish rule, deportations of Chechens, Ingush and other ethnic groups during Stalinism).

The locals are partly Muslims, some Orthodox Christians (Russians, Ossetians, Georgians, some Kabardians), as well as Monofisites (Armenians). The Armenian Church and the Georgian Church are among the oldest Christian churches in the world. Both churches have an extremely important role in promoting and protecting the national identity of peoples who have been under foreign rule for two centuries (Turks, Persians).

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.
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.

Caucasus Mountains on the border of Russia and Georgia