Where are the Caucasian mountains on the map. Variants of the highlands of Russia. Location of states in the Caucasus

In the ridge of the Caucasus Mountains is Elbrus. It is also considered the whole of Europe. Its location is such that several peoples live around it, who call it differently. Therefore, if you hear such names as Alberis, Oshkhomakho, Mingitau or Yalbuz, know that they mean the same thing.

In this article, we will introduce you closer to the most high mountain in the Caucasus - Elbrus, which was once active volcano, and occupying the fifth place on the planet, among the mountains formed in the same way.

The height of the Elbrus peaks in the Caucasus

As already mentioned, the highest mountain in Russia is dormant volcano. This is precisely the reason why its top does not have a pointed shape, but looks like a two-peak cone, between which there is a saddle at an altitude of 5 km 200 m. Two peaks located at a distance of 3 km from each other are different: the eastern one is 5621 m, and the western one is 5642 m. The reference always indicates a great value.

Like all former volcanoes, Elbrus consists of two parts: a pedestal made of rocks, in this case it is 700 m, and an artificial cone formed after eruptions (1942 m).

Starting from a height of 3500 m, the surface of the mountain is covered with snow. First, mixed with scatterings of stones, and then turning into a uniform white cover. by the most famous glaciers Elbrus are Terskop, Big and Small Azau.

The temperature at the top of Elbrus practically does not change and is -1.4°C. Drops out here a large number of rainfall, but because of this temperature regime, it is almost always snow, so the glaciers do not melt. Since the snow cap of Elbrus is visible all year round for many kilometers, the mountain is also called "Small Antakrtida".

The glaciers located at the top of the mountain feed the most big rivers these places - Kuban and Terek.

To see beautiful view, opening from the top of Elbrus, you need to climb it. It is quite simple to do this, since you can get to a height of 3750 m along the southern slope on a pendulum or chairlift. cable car. Here is a shelter for travelers "Barrels". It consists of 12 insulated trailers for 6 people and a stationary kitchen. They are equipped so that they can wait out any bad weather, even for a long time.

The next stop is usually made at an altitude of 4100 m in the Shelter of Eleven Hotel. The parking lot here was established in the 20th century, but was destroyed by fire. Then a new building was built in its place.

For the first time, the peaks of Elbrus were conquered in 1829 on the east and in 1874 on the west.

Now the Donguzorun and Ushba massifs, as well as the Adylsu, Adyrsu and Shkheldy gorges are popular with climbers. Increasingly, mass ascents to the peaks are organized. WITH south side located ski resort Elbrus Azau. It consists of 7 tracks, with a total length of 11 km. They are suitable for both beginners and advanced skiers. A distinctive black of this resort is freedom of movement. On all routes there is a minimum number of fences and dividers. It is recommended to visit it from October to May during this period there is the strongest snow.

Elbrus is at the same time very beautiful and dangerous mountain. Indeed, according to scientists, there is a possibility that in the next 100 years the volcano will wake up, and then all nearby regions (Kabardino-Balkaria and Karachay-Cherkessia) will suffer.

The Caucasus Mountains are a mountain system between the Black, Azov and Caspian Seas. The etymology of the name has not been established.

It is divided into two mountain systems: the Greater Caucasus and the Lesser Caucasus.

The Caucasus is often divided into North Caucasus and Transcaucasia, the border between which is drawn along the Main, or Dividing Range Greater Caucasus, which occupies a central position in mountain system.

The Greater Caucasus stretches for more than 1,100 km from the northwest to the southeast, from the Anapa region and the Taman Peninsula to Absheron Peninsula on the Caspian coast, near Baku. Max Width The Greater Caucasus reaches in the region of the Elbrus meridian (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 extend ( mountain ranges), including a monoclinal (cuest) character (see Greater Caucasus). Southern slope of the Greater Caucasus for the most part consists of echelon-shaped ridges adjacent to the Main Caucasian ridge. Traditionally, the Greater Caucasus is divided into 3 parts: Western Caucasus(from the Black Sea to Elbrus), Central Caucasus(from Elbrus to Kazbek) and the Eastern Caucasus (from Kazbek to the Caspian Sea).

Countries and Regions

1. South Ossetia
2. Abkhazia
3. Russia:

• Adygea
• Dagestan
• Ingushetia
• Kabardino-Balkaria
• Karachay-Cherkessia
• Krasnodar region
• North Ossetia Alania
• Stavropol region
• Chechnya

Cities of the Caucasus

• Adygeysk
• Alagir
• Argun
• Baksan
• Buynaksk
• Vladikavkaz
• Gagra
• Gelendzhik
• Grozny
• Gudauta
• Gudermes
• Dagestan lights
• Derbent
• Dusheti
• Essentuki
• Zheleznovodsk
• Zugdidi
• Izberbash
• Karabulak
• Karachaevsk
• Kaspiysk
• Kvaisa
• Kizilyurt
• Kizlyar
• Kislovodsk
• Kutaisi
• Leningor
• Magas
• Maykop
• Malgobek
• Makhachkala
• Mineral water
• Nazran
• Nalchik
• Nartkala
• Nevinnomyssk
• Novorossiysk
• Ochamchira
• Chill
• Pyatigorsk
• Stavropol
• Stepanakert
• Sukhum
• Urus-Martan
• Tbilisi
• Terek
• Tuapse
• Tyrnyauz
• Khasavyurt
• Tkuarchal
• Tskhinvali
• Cherkessk
• Yuzhno-Sukhokumsk

Climate

The climate in the Caucasus varies both vertically (altitude) and horizontally (latitude and location). The temperature usually decreases with elevation. The average annual temperature in Sukhum, Abkhazia at sea level is 15 degrees Celsius, and on the slopes of the mountains. Kazbek at an altitude of 3700 m, the average annual air temperature drops to -6.1 degrees Celsius. On the northern slope of the Greater Caucasus Range it is 3 degrees Celsius colder than on the southern slopes. In the highlands of the Lesser Caucasus in Armenia, Azerbaijan and Georgia, a sharp temperature contrast between summer and winter is noted due to a more continental climate.

Precipitation increases from east to west in most areas. Altitude plays an important role: the Caucasus and the mountains usually receive more precipitation than the lowlands. Northeast regions(Dagestan) and South part Lesser Caucasus are dry. The absolute minimum of annual precipitation is 250 mm, in the northeastern part Caspian lowland. West Side The Caucasus is characterized by high rainfall. There is more precipitation on the southern slope of the Greater Caucasus Range than on the northern slopes. Annual precipitation in the western part of the Caucasus ranges from 1000 to 4000 mm, while in the Eastern and North Caucasus (Chechnya, Ingushetia, Kabardino-Balkaria, Ossetia, Kakheti, Kartli, etc.) the amount of precipitation ranges from 600 to 1800 mm . The absolute maximum of annual precipitation is 4100 mm in the region of Meskheti and Adjara. The level of precipitation in the Lesser Caucasus (southern Georgia, Armenia, western Azerbaijan), not including Meskhetia, varies from 300 to 800 mm per year.

The Caucasus is famous big amount snowfall, although many regions that are not located along slopes to windward do not receive much snow. This is especially true for the Lesser Caucasus, which is to some extent isolated from the influence of humidity coming from the Black Sea and receives much less precipitation (in the form of snow) than in the mountains of the Greater Caucasus. On average, in winter, snow cover in the mountains of the Lesser Caucasus ranges from 10 to 30 cm. Heavy snowfalls are recorded in the mountains of the Greater Caucasus (in particular, on the southwestern slope). Avalanches are a frequent occurrence from November to April.

Snow cover in some regions (Svaneti, in the northern part of Abkhazia) can reach 5 meters. The Achishkho region is the snowiest place in the Caucasus, the snow cover of which reaches a depth of 7 meters.

Landscape

The Caucasus Mountains have a varied landscape that mostly varies vertically and depends on 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).

On the northern slopes of the Greater Caucasus for more low altitudes oak, hornbeam, maple and ash are common, and birch and pine forests. Some of the most low 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 high 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 m.

(Visited 1 238 times, 1 visits today)

The Caucasus is a mountain system located in Eurasia between the Black and Caspian Seas. The mountain chain stretches for 1100 km from the Taman Peninsula and Anapa to the Absheron Peninsula near the city of Baku.

It is customary to divide this territory according to several criteria: into the Greater and Lesser Caucasus, as well as into the Western (from the Black Sea to Elbrus), Central (from Elbrus to Kazbek) and Eastern (from Kazbek to the Caspian Sea). The mountain system reaches its greatest width in the central part (180 km). The mountain peaks of the Central Caucasus are the highest on the Main Caucasian (Dividing) Range.

The most famous Mountain peaks The Caucasus is Mount Elbrus (5642 m) and Mount Kazbek (5033 m). Both peaks are stratovolcanoes. Moreover, Kazbek is considered to be extinct, which cannot be said about Elbrus. The opinions of experts on this matter vary. The slopes of the two highest mountains of the Caucasus are covered with snow and glaciers. The Central Caucasus accounts for up to 70% of modern glaciation. For more than a century of observations of the glaciers of the Caucasus, their area has significantly decreased.

To the north, from the foot of the Greater Caucasus, an inclined plain extends, which ends with the Kumo-Manych depression. Its territory is dissected by lateral ridges and river valleys. by the most major rivers this area can be considered Kuban and Terek. To the south of the Greater Caucasus are the Colchis and Kura-Araks lowlands.

The Caucasus Mountains can be considered young. They were formed in the era of Alpine folding about 28-23 million years ago. Their formation is due to the movement of the Arabian lithospheric plate to the north to the Eurasian one. The latter, pressed by the African plate, moves several centimeters a year.

Tectonic processes in the depths of the Caucasus continue to this day. Geological structure Elbrus speaks of the great activity of the volcano in the recent past. Several powerful earthquakes occurred in the Caucasus in the 20th century. The most devastating was the earthquake in Armenia in 1988.

Seismic stations operating throughout the Caucasus annually register several hundred earthquakes. Experts say that some sections of the Caucasus Range "grow" by several centimeters per year.

Caucasus in Europe or in Asia?

This issue should be considered more in political and historical aspects. The Caucasus Mountains are located in the center of the Eurasian Plate, so the division can only be conditional. The border between Europe and Asia was proposed by the Swedish officer and geographer F. Stralenberg in 1730. The border that passed along Ural mountains and the Kuma-Manych depression was accepted by many scientists.

Despite this, in different time several alternative proposals were proposed that justified the division of Europe and Asia along the Caucasus Mountains. Despite ongoing disputes, Elbrus is still considered the highest point in Europe. The history of the region suggests the special position of the Caucasus at the crossroads between European and East Asian cultures.

The highest mountains of the Caucasus

• Elbrus (5642 m). KBR, KChR. Highest point Russia
• Dykhtau (5204 m). CBD
• Koshtantau (5122 m). CBD
• Pushkin Peak (5100 m). CBD
• Dzhangitau (5058 m). CBD
• Shkhara (5201 m). CBD. The highest point of Georgia
• Kazbek (5034 m). The highest point of North Ossetia
• Mizhirgi Western (5022 m). CBD
• Tetnuld (4974 m). Georgia
• Katyntau (4970 m). CBD
• Peak Shota Rustaveli (4960 m). CBD
• Gestola (4860 m). CBD
• Jimara (4780 m). Georgia, North Ossetia
• Ushba (4690 m). Georgia, North Ossetia
• Gulchitau (4447 m). CBD
• Tebulosmta (4493 m). The highest point of Chechnya
• Bazarduzu (4466 m). The highest point of Dagestan and Azerbaijan
• Shan (4451 m). The highest point of Ingushetia
• Adai-Khokh (4408 m). North Ossetia
• Diclosmta (4285 m). Chechnya
• Shahdag (4243 m). Azerbaijan
• Tufandag (4191 m). Azerbaijan
• Shalbuzdag (4142 m). Dagestan
• Aragats (4094). The highest point of Armenia
• Dombay-Ulgen (4046 m). KCHR

How many five-thousanders are in the Caucasus?

It is customary to call Caucasian five-thousanders mountains whose height exceeds five kilometers. From the list above, it is clear that Caucasus eight mountains "five-thousanders«:

• Elbrus(5642 m) is a dormant volcano and the highest mountain in Russia. The mountain consists of two peaks Western (5642 m) and Eastern (5621 m), connected by a saddle (5416 m).
• Dykhtau(5204 m) - mountain peak of the Lateral Range of the Greater Caucasus. The mountain consists of two peaks (both over 5000 m high), connected by a steep narrow saddle. The first ascent to the mountain took place in 1888. To date, about ten routes have been laid to the top of Dykhtau with a difficulty of 4A (according to the Russian classification).
• Koshtantau(5122 m) - a mountain peak on the border of Bezengi and mountainous area Balkaria.
• Pushkin Peak(5100 m) - being part of mountain range Dykhtau, is a separate peak. Named after A.S. Pushkin to the 100th anniversary of his death.
• Dzhangitau(5058 m) - a mountain peak in the central part of the Greater Caucasus. There are three peaks in the Dzhangitau massif, all of which have a height of more than five kilometers.
• Shkhara(5201 m) - a mountain peak of the Central Caucasus, which is part of the Bezengi wall.
• Kazbek(5034 m) is an extinct stratovolcano, the easternmost five-thousander of the Caucasus. The first ascent of the mountain was made in 1868.
• Mizhirgi Western(5022 m) - a mountain peak as part of the Bezengi wall. The name of the mountain is translated from Karachay-Balkar as "connecting".

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 a 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." The length of the 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 due to the relief, which is represented by different forms. Mountain peaks with sharp peaks shot up under the very sky. 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. on the south and western slopes much more precipitation than on the northern and eastern slopes. The Caucasus Mountains are located in almost all climatic zones: from humid subtropics with humid and warm winter, 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, mountain jerboa and ground squirrel, and bears and leopards live in remote places. On the way from the foot to the top, meadow alpine grasses grow and coniferous forests, which "feed" on rivers, lakes, waterfalls, springs with mineral waters.

• For the first time, a man climbed the highest high peak system 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.

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 the mountain system. 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 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).

The 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). major centers glaciations 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 in the west of the southern part of the Caucasus is the Transcaucasian Highlands, which consists of the ranges of the Lesser Caucasus and the Armenian Highlands (Aragats, 4090 m). Lesser Caucasus connects with Greater Caucasus Likhsky 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 winter Olympic Games 2014.