We describe the Caucasian mountains on the map. Caucasian mountains

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 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 ridges (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).

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. The northeastern regions (Dagestan) and the southern part of the Lesser Caucasus are dry. The absolute minimum of annual precipitation is 250 mm in the northeastern part of the Caspian lowland. The western part of 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 known for a high amount of 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).

Oak, hornbeam, maple and ash are common on the northern slopes of the Greater Caucasus at lower altitudes, and birch and pine forests. 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 m.

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Greater Caucasus- a mountain system between the Black and Caspian Seas. It extends 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 highest peak is Elbrus (5642 m).

The state border of the Russian Federation with Abkhazia, Georgia, South Ossetia and Azerbaijan passes through the Greater Caucasus.

Scheme of the ridges of the Greater Caucasus. Volcanoes are marked with red circles.

The Greater Caucasus, together with the Lesser Caucasus, makes up the Caucasus Mountains and is separated from the latter by the Colchis and Kura-Araks lowlands and the Kura valley in the middle reaches between them.

The Greater Caucasus reaches its maximum width in the Elbrus region (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 - the Side Range, the Rocky Range, etc.

Parts and districts

View from Ushba to Elbrus. Photo by O. Fomichev.

Traditionally, the Greater Caucasus is divided into 3 parts:

Table 1. The peaks of the Caucasus are higher than 4700 m (bold font indicates the height according to the topographic map at a scale of 1:50000).

N Peak name Height Part of BC Area
1 Elbrus 5642 Central Elbrus region
2 Dykhtau 5205 Central Bezengi
3 Shkhara 5203 Central Bezengi
4 Koshtantau 5152 Central Bezengi
5 Dzhangitau 5085 Central Bezengi
6 Kazbek 5034 Central Prikazbeche
7 Mizhirgi 5019 Central Bezengi
8 Katyntau 4979 Central Bezengi
9 Gestola 4860 Central Bezengi
10 Tetnuld 4858 Central Bezengi
11 Jimaraikhoh 4780 Central Tepli-Dzhimaraisky
12 Ushba 4700 Central Elbrus region

Climate

Rest in the Adish Icefall. Photo by A. Lebedev (1989)

The climatic features of the Greater Caucasus are determined by the altitudinal zonality and the rotation of the mountain barrier formed by it at a certain angle to the western moisture-bearing air flows - the Atlantic cyclones and the Mediterranean western air currents of the middle layers of the troposphere. This rotation has a decisive influence on the distribution of precipitation.

The wettest is the western part of the southern slope, where more than 2500 mm of precipitation falls annually in the highlands. The record amount of precipitation falls on the Achishkho ridge near Krasnaya Polyana - 3200 mm per year, this is the wettest place in Russia. Winter snow cover in the area of ​​the meteorological station Achishkho reaches 5-7 meters!

N Name of the glacier Length km Area sq. km end height Firn line height Area
1 Bezengi 17.6 36.2 2080 3600 Bezengi
2 Karaug 13.3 34.0 2070 3300 Karaug
3 Dykh-Su 13.3 26.6 1830 3440 Bezengi
4 Lekzyr 11.8 33.7 2020 3090 Elbrus region
5 Big Azau 10.2 19.6 2480 3800 Elbrus region
6 zanner 10.1 28.8 2390 3190 Bezengi

Glaciation is especially significant in the Central Caucasus and in the eastern part of the Western Caucasus. In the Eastern Caucasus, small glaciers are found only in individual high mountain nodes.

They are no less famous in the world than the Cordillera, a mountain system that stretches along the western outskirts of North and South America for as much as eighteen thousand kilometers in length and in width for 1600 kilometers, with the highest peak of Denali at 6190 meters above sea level in North America, also in Aconcagua - 6963 meters above sea level in South America. Many countries border the Cordillera - Mexico, Venezuela, Colombia, Ecuador, Peru, Bolivia, Argentina and Chile. No less famous is the Cordillera mountain system of the Himalayas with the highest peak Chogori - 8611 meters above sea level on the border of China and Pakistan and with another peak Lhotse, exceeding a height of eight kilometers on the border of China and Nepal. On the globe, Tibet is also admired with the highest peak in the world, Everest - 8852 meters above sea level. However, on Earth there are other mountain systems on different continents that attract attention and which thousands and thousands of brave conquerors of peaks strive to climb.

From the legendary Taman to the gray Caspian

The Great Caucasus Mountains are essentially two mountain systems - the Greater and Lesser Caucasus in Eurasia. They stretched for more than 1,100 kilometers from northwest to southeast, and more specifically, from the Taman Peninsula in the region and along the Black Sea coast to the Absheron Peninsula near the gray Caspian and near the capital of Azerbaijan, Baku. The maximum width of the mountain system is 180 kilometers. Compared to the Cordillera, this is almost a ninth, but nevertheless noticeable and being the root cause of the appearance of a subtropical zone in Russia. In which over 15 million of our fellow citizens and guests from near and far abroad improve their health and have a good rest every year. The Greater Caucasus is divided into three parts: Western - from the Black Sea to Elbrus; Central - from Elbrus to Kazbek and finally the Eastern Caucasus - from Kazbek to the Caspian Sea. As for the height above sea level, then at Everest it is 5642 meters, at Kazbek 5033. The total area of ​​the Great Caucasus mountains 1400 square kilometers. In part, this is the land of eternal snows and glaciers. The area of ​​glaciers goes off scale for 2050 square kilometers. A major center of icing is Mount Elbrus plus the Bezengi wall - 17 kilometers.

The land of five dozen nations

The Great Caucasus Mountains are densely populated. Meaning its foothills. Abkhazians, Ingushs, Ossetians, Armenians, Azerbaijanis, Adygs (Circassians) and many other nationalities live here, united by a common name - the Caucasian peoples. Most of them are Muslims. But Christians are also widely represented - Ukrainians, Georgians, Russians, Armenians, as well as a noticeable part of Ossetians and Abkhazians. By the way, Armenian and Georgian churches are the oldest in the world. Thanks largely to them, these two peoples of the Great Caucasus have retained their identity, customs and customs. Let's add to this - Caucasian peoples for a hundred years they were under foreign control - Turks, Persians, Russians. Now others have gained independence, become sovereign.

twenty-five sky-high peaks

That is how many of them the Great Caucasus has from Elbrus to Dombay-Ulgen - 4046 meters above sea level. Popular with climbers: Dykhtau - 5204 meters above sea level; Pushkin peak - 5100 m., we have already mentioned Kazbek; Shota Rustaveli - 4960m., Gulchi-Tau - 4447 meters, etc.

The Great Caucasus is abundant in rivers, lakes and waterfalls

Originating at the mountain peaks, some flow into - Bzyb, Kodor, Ingur (Inguri), Rioni, Mzymta, etc. B - the largest Kuban in the Krasnodar Territory. And in the Caspian - Kura, Samur, Terek, Sunzha, Baksan - there are more than two dozen of them in total. Among the majestic Caucasus Mountains is the world-famous Lake Sevan (Armenia). It is located at an altitude of 1900 meters above sea level. Its area is 1240 square kilometers, the depth is from twenty to over eighty meters. 28 rivers flow into the lake, but only one flows out - Hrazdan, a tributary of the Araks. By the way, it will be noticed - both the Caspian and Black Sea the essence of the remnant of the once world ocean Tethys. The names of the Black Sea have changed since ancient times - Khazar, Sugde, Temarun, Cimmerian, Akhshaena, Blue, Tauride, Holy and even Ocean. The current name is due to its color in raging storms. It really does look black. In the old days, he was also fearfully called not hospitable, angry. The Caspian reservoir got its name from the tribes of horse breeders who once lived near its shores - the Caspians. It was also called Girkansky, Dzhurazhansky, Khvalynsky, Derbent - more than seven dozen names in total.

And about one more unique water body of the Great Caucasus - the Zeygalan waterfall, which is fantastic in terms of natural beauty (otherwise it is also called the Great Zeygelan waterfall). It is located in North Ossetia in the valley of the Midagrabindon River, seven kilometers south of the village of Dzhimara. The height of the fall is 600 meters. Translated from Ossetian - "falling avalanche". It is one of the ten most grandiose and famous waterfalls in the world. It pushes back fellow Gavarni in France - 422 meters high and Krimml in Austria - 380 meters. It originates from under the hanging glacier at an altitude of 650-700 meters. The peak flow occurs in the summer months of July-August. In winter it dries up and is marked only by ice smudges on the rocks. The waterfall area is part of the Kazbek-Dzhimarai mountain junction, the largest not only in North Ossetia, but in the entire Great Caucasus. The place is delightful in its beauties - on the slopes of the mountains, a sea of ​​​​flowers, herbs, aromas of alpine meadows are dizzy. But you should be careful - the waterfall is dangerous for people: rockfalls happen, sometimes pieces from a melting glacier fly from above. Nevertheless, the waterfall is actively visited. Tourists shoot a grandiose panorama of the waterfall with a camera or TV camera.

Flora and fauna of the Great Caucasus

As for the flora, it is represented by almost six and a half thousand flowering plants. Of these, 166 are unique to mountains. The subtropics are famous for dozens of palm species. Relic juniper and pistachio grow here; Pitsunda pine, oaks, hornbeams, mimosa, tulip tree, magnolias, bamboo - you can’t list all the tree species. Individual patriarchal oaks over a thousand years old. Tourists are advised to walk in the juniper groves. Especially for those with asthma or bronchitis. The breath of juniper kills all microbes and viruses in a person in minutes. A day, two, three walks, and you seem to be born again! This is also facilitated by sea air, thickly infused with salts of bromine, calcium, potassium, etc.

As for the fauna of the Great Caucasus Mountains, it is also rich and diverse here. You will also come across wild boars (beware of mothers and fathers with cubs: the fangs of males are sharp, and there were cases when a meeting with wild boars ended in serious injuries or, worse, death!). There are also chamois, mountain goats, and bears. Once lived both lynxes and leopards. Asiatic lions and tigers. The Caucasian bison became extinct in 1925. The last elk was killed in 1810. A great variety of invertebrates - only spiders in a thousand species. The Great Caucasus is also the habitat of golden eagles, which are caught by poachers and sold abroad for big money. They like to hunt with golden eagles in the Caucasus itself, and in Kazakhstan, and in Kyrgyzstan, and in Saudi Arabia, in other regions and countries of the planet.

Stele of the Soaring Eagle

It appeared in 2013 near the resort villages and Supsekh, not far from Varvarovka, from where the Turkish Stream gas pipeline originates, and was opened as a race for the Day of Russia. Nine kilometers from Anapa. The authors are the sculptor V. Polyakov in collaboration with the architect Y. Rysin.

The monument is made of cold bronze, which guarantees its durability and which is not afraid of any weather changes. A soaring eagle with a wide wingspan and head proudly raised to the sky means the beginning of the Great Caucasus Mountains. In front of the stele there is a platform for vehicles. Tourists, and here they are, passing to other resort villages of Bolshoi and Maly Utrish, thousands and thousands will definitely stop and take pictures or film the monument on a video camera. By the way, the "Soaring Eagle" offers a stunning view of Anapa and the bays, in which the city is freely spread out (in ancient times, he wore a mysterious ancient Greek name Gorgippia, and the slave trade was actively conducted in it, their own coins were minted, and representatives of the nobility from different regions of the Caucasus came and sailed here for white-faced brides!). In good weather, the coast is visible right up to the bank of Mary Magdalene, which is near the village - and where divers come and flock not only from all over Russia, but also from abroad. So, the Great Caucasus Mountains begin from the foothills and, in particular, from Bald Mountain with a height of only 319 meters above sea level, other hills are even lower. The foothills enter the very beginning of the Semisamsky ridge, which is part of the chain of the Caucasus Mountains. And Bald Mountain is called because of the absence of any vegetation on it at all. No, no, herbs and flowers are found there. But not more. Let us remind you once again - from the center of Anapa to Bald Mountain is nine kilometers, and from the outskirts of the city it is three times less. And with your hand, as they say, file up to the Small and. And these places are well known to tourists.

Near Bolshoi Utrish, one of the main attractions of the beginning of the Great Caucasus is a dolphinarium on the high seas and with a theater. During the high season, several performances are given daily. Artists are sea animals. Towards the end of a kind of performance, bottlenose dolphins deftly jump onto the platform and willingly take pictures with everyone or filmed on a television camera. You can hug them heartily, kiss them or swim in the waters of the dolphinarium. Meanwhile, the seal, leaning on its tail, recklessly applauds the audience with its flippers. On the Big Utrish, according to legends, the hero Prometheus was chained to one of the rocks, who gave people the sacred fire and thereby caused fierce anger from the main god of Olympus, Zeus the Thunderer. Zeus ordered the disobedient to be chained to a rock with strong chains, and a bloodthirsty eagle flew to the martyr to torment his liver with sharp claws. True, residents of neighboring Sochi, Anapa, object, de Prometheus was chained in the Eagle Rocks area near the former capital of the Winter Olympic Games 2014. And they even built a monument to the hero - Prometheus is standing on a mountain with chains torn in his hands, and he has a proud look of a winner! And yet, the assertion of the Sochi residents raises doubts: Eagle Rocks are located far from the sea, near a fast river. But in the museum under open sky in the center of Anapa "Gorgippia" they found a crypt with frescoes of the exploits of another mythological hero - Hercules. And from the myths Ancient Greece it is known for certain that it was Hercules who freed Prometheus from the chains. He drove the bloodthirsty eagle away. Who is right and who is wrong - let the experts decide. But in Anapa, which is no less than two and a half thousand years old, they stubbornly believe that the rock of Prometheus is still located on Bolshoi Utrish. In their opinion, another legend is irrefutable - de the Argonauts, led by their brave captain Jason, sailed past the rocks of the Big Utrish in search of the Golden Fleece. These are the secrets shrouded in the beginning of the Great Caucasus Mountains near Anapa and the stele of the Soaring Eagle.

Peaks from Novorossiysk to Gelendzhik

Today there are five resort areas: Sochi, Gelendzhik, Tuapse, Anapa and Taman. From each of them to the other, as they say, within easy reach. And all of them stretched along the Black Sea coast with the exception of Taman, which also has access to the Sea of ​​Azov. And the Black Sea coast is mostly protected by mountains. Except for Anapa, where, as we have noticed, the Great Caucasus Mountains begin, but in general the municipality goes from the sea to the steppe expanses. And only in the region of Novorossiysk, as a continuation of the Semisamsky ridge with Lysa Gora, the foothills gradually rise, passing into the Markotkhsky ridge or on the Adygsky to Markotkh, stretching from Novorossiysk towards Gelendzhik for more than ninety kilometers. The highest mountain towering over Novorossiysk is Sugarloaf (558 meters above sea level). Gradually rising, the Markotkhsky ridge in some places goes up more than 700 meters. It consists of limestone, sandstone, clay, but its main component is marl, which is used to make cement. This is especially noticeable near Novorossiysk - factories for the production of this type of building materials are operating, and dust is around the pillar. Markotkhsky ridge, we note, runs parallel to and south of the Main Caucasian ridge. There are many sights between Novorossiysk and Anapa. In particular, the natural monument is the Sheskharis juniper forest. ABOUT healing properties relic juniper we told above, therefore we will not repeat ourselves, we only emphasize that it is especially useful in the treatment of asthma and bronchi. From Anapa to Novorossiysk directly 40 kilometers, along the highway - 52. You can overcome them in a little more than forty minutes. And if you drive another 14 kilometers towards Gelendzhik, then you will find yourself on the Abrau Peninsula, at the southern end of which is Bolshoi Utrish with its famous dolphinarium on the high seas and a theater. But the main feature of the peninsula is undoubtedly the place Abrau-Dyurso, comfortably located among the mountains and part of municipality resort city of Novorossiysk.

Specific estate of Russian sovereigns

The village has a double name -. And this has its own reason. One village is located in the mountains, among fantastically beautiful nature. There is a river of the same name and the largest freshwater lake in the Caucasus with the same name as the village. With a population of about three thousand, living like in paradise. Mild climate, warm winters and vineyards, vineyards, vineyards. Lake Abrau is 3100 meters long, 630 meters wide, 8 to 11 meters deep, by the way, there are fish in it. Gorgeous embankment - with gazebos, benches. In summer, the water is warm, and you can swim in the lake with pleasure. But you can plunge into the Black Sea. At the second village of the royal estate - Durso. Today there are recreation centers and health resorts where you can relax and get medical treatment.

The village of Abrau is known in the world for its exquisite taste of Russian champagne. At the origins of its production was Prince Lev Golitsyn. And the baton was picked up, surprisingly, by Joseph Stalin, who ordered the production of domestic champagne in the southern regions of the country and in Abrau, in particular. And such an indication of his was contained in a government decree of 1936. As for the production of champagne under the patronage of Golitsyn, its first batch was produced in 1898. And two years later, a powerful winery appeared in Abrau. A highway was laid from Novorossiysk to the village. Now in Abrau there is a museum of famous wines, as well as a company store where tourists can buy Russian champagne under the Abrau-Durso brand, dry wines and even cognac if they wish. There are many entertainments on the coast in Durso - water rides, "bananas", "pills", you can rush through the waves on jet skis with a breeze. And in Abrau, horseback riding along the local foothills, mountain tourism, including jeeping or extreme trips, but already on mountain bikes, are popular.

Markoth near Gelendzhik

To the famous no less than Anapa, a resort from Novorossiysk, the distance is mere trifles - directly three dozen kilometers, ten kilometers more along the highway. The trip will take somewhere a little over forty minutes. And now you will see the longest embankment in the world - 14 kilometers. With a graceful figure of a bride made of white marble, which is clearly visible from the height of the Markoth Range at 762 meters above sea level. Translated from the Adyghe "Markotkh" literally means "berry places", and here you can collect really tasty blackberries in buckets. It pricks, it's true, but what is called "you can't even catch a fish from a pond without difficulty!". There are several high peaks in the vicinity of Gelendzhik - Shakhan near the Zhane River (700 meters above sea level); Pshada - 741 meters near the river of the same name and 43 kilometers long, flowing into the Black Sea; Gebius - 735 meters above sea level. The Markothsky Range itself stretches along the Gelendzhik Bay - charmingly beautiful from a bird's eye view, and even more so from the tops of the surrounding mountains. The resort is famous for its Safari Park, where lions, tigers, bears and other animals live in natural conditions. You can also watch their life from the chairlift. At the top of the Mrkotkh Ridge - a fantastic forest - with a goblin, a mermaid on the branches of a tree, Baba Yaga and others fairy tale characters. From the observation deck, yachts and other vessels in the bay, gulls, cormorants, petrels, soaring over the blue sea with white crests of waves, are clearly visible.

And the mountains are getting higher, and the mountains are getting steeper!

And this is true if you go from Gelendzhik to the Bolshoi - the southern capital of Russia, stretching along the Black Sea coast for as much as one hundred and forty-five kilometers. There is only one city in the world longer than the former capital of the last Winter Olympic Games, in which our team triumphantly won and which amazed the planet with their colorful opening and closing ceremonies - the capital of Mexico, Mexico City - 200 kilometers. And in the native Fatherland, Sochi is ahead of Volgograd in length, stretching along great river Volga for more than 90 kilometers. So about the height of the local mountains. Having overcome the distance from Gelendzhik to Sochi of 246 kilometers in almost four hours (the game is worth the candle!), You can climb, including as part of excursion groups, one of the surrounding peaks. You can start small - Mount Akhun - 663 meters above sea level. And then the height of the mountains will increase: Sugar, fifteen kilometers from the city - 1555 meters; Przegishva - 2216 meters; Big Weaver - 2368 meters; Achishkho - 2391 meters; Bzerli peak - 2482 meters; Perevalnaya South - 2503 meters; Stone pillar - 2509 meters; Pshekho-Su - 2743 meters; Oshten - 2804 meters; Fisht - 2853 meters; Peak Kozhevnikov - 3070 meters; Peak Needle - 3168 meters; Sugar Pseashkho - 3189 meters; Atheist - 3256 meters and finally the highest peak of the entire Kuban Tsakhvoa - 3346 meters above sea level. This is not so little, considering that the highest peak of the Great Caucasus Mountains and even Europe is Elbrus, 5642 meters above sea level.

The famous ski resort "Krasnaya Polyana"

It is located in the middle reaches of the mountain river Mzymta, which is translated from the Adyghe - "mad", uncontrollable", "indomitable" - there are other interpretations. It flows into the Black Sea. It is 39 kilometers long. Over the gorge above it, the famous pedestrian suspension bridge is the most longest in the world. From it, extreme sports lovers jump into the abyss on an elastic cable. Here, a popular attraction is a giant swing with a pendulum span of half a kilometer. From the west near Mount Achishkho, from the east - the Aibga ridge. Immediately in the vicinity is Fisht peak, in honor of which was named the stadium where the opening and closing ceremonies of the Winter Olympic Games were held in 2014. Krasnaya Polyana is a ski resort that can compete with its counterparts in the same Switzerland or in other mountainous places on the planet. They have at their disposal more than a hundred kilometers of snow slopes of various difficulty levels - 6 green, 8 blue, 16 red and 6 black. Experienced skiers and beginners and children can feel it. Among independent ski resorts- "Rosa-Khutor", "Alpika-Service", "Gorki Gorod" and GTZ "Gazprom". Skiing during the day, discos, karaoke in the evening, pleasant evenings in cafes, restaurants, casinos. There will be enough places for everyone - hotels, guest houses, you can rent a cottage. There are no problems with transport. Adler is forty kilometers away. You can fly there by direct flights from many regions of Russia. And then rail transport with the famous "Swallows", or regular buses, even faster personal cars. The road will not seem tedious to you. Especially with such fantastic natural beauties! By the way, in Krasnaya Polyana there are enough bases for renting skis, snowboards, sleds and so on.

Arriving in Sochi for rest and treatment (it receives more than five million tourists a year, not including those who prefer snow slopes that operate from November to April inclusive, and sometimes taking the beginning of May), be sure to visit the Olympic Park. It is located near the Black Sea. With the stadium "Fisht" and other sports facilities built for the White Olympics. All of them have unique architecture. The Ice Palace resembles the Beijing Opera - in the form of an icy drop. And the Olympic cauldron! She looks like the Firebird from Russian folk tale. In the Olympic Park there is a Formula 1 track, and the competition for pilots leaves no one indifferent. Fans come from all parts of the world and remain in great delight. The park has its own "Disneyland" with dozens of rides. Souvenirs, including the mascots of the Games, can be bought as a keepsake in local places. Just keep in mind - you can't get around the park in one day. It covers an area of ​​almost two hundred hectares. In the Imeretinskaya lowland. Do not go around it in a day and on electric cars: there are so many sights in it. Natural beauty of Tuapse

Famous resort town located between Gelendzhik and Sochi. It is 117 kilometers away from the southern capital of Russia - less than two hours away. From Gelendzhik - 129 kilometers, a little over two hours drive. The mountains that protect the resort from the evil northern winds, on average, are from 1352 to 1453 meters above sea level. But there are exceptions - the top of Chessy ascended to the sky at 1839 meters. Among the attractions are Mount Semiglavaya, the Wolf Gorge, the rock of Alexander Kiselev, protruding into the sea and named after the artist. In the city itself - subtropical plants. in the foothills and locals and tourists are happy to collect European blackberries. In the resort area there are sanatoriums, boarding houses, children's health camps. Both cargo and passenger ships moor in the seaport. You can rent a yacht, go to the open sea on it, go fishing, swim in the clearest water or sunbathe on the deck. Tourists love to arrange picnics during boat trips.

Republic of Adygea

It is part of the South Federal District with the capital Maykop with a population of half a million. Part of the North Caucasian economic region. Surrounded on all sides Krasnodar Territory. There are forty-five auls in the republic, there are villages, villages, farms. From the streets of Maykop, the Main Caucasian Range is clearly visible. Sights - Lago-Naki plateau, popular with tourists. Ten waterfalls Rufabgo - each with its own name. Rivers Kuban, Belaya, Laba. The Belaya River is 260 kilometers long. And it is fed by mountain streams and springs of Fisht, Oshten and Abago. The granite canyon is four kilometers long and two hundred meters deep. Sahrai waterfalls. Mountain lake Pseudonakh. Often visited by tourists are the Devil's Finger rock, Monk, Big Weaver, Trident, Camel, Una-Koz ridge. The mountains are quite high, we recall that the top of Fisht ascended to 2868 meters above sea level. It was her name that was given to the stadium where the opening and closing ceremonies of the Winter Olympic Games in 2014 took place, so striking with their colorfulness and originality inherent in the Russian mentality.

Dagestan - a country of mountains

On this account, there are folk saying. It is especially often used in speeches on December 11, when the whole world celebrates International Mountain Day. And the highest of the peaks of the Great Caucasus here - Shalbuzdag - 4150 meters above sea level. In July and August, there is a real pilgrimage to her: here is the grave of the righteous Suleiman. The mountain resembles a pyramid with a jagged top. There is a belief that if you climb it, all desires and dreams will come true. And thousands of tourists are trying to do it. But the capital of Dagestan, Makhachkala, stretches directly along the Tarki-Tau mountain - a unique natural monument from a mountain monolith. It is also well known because in 1722 the army of Peter the Great entered Tarki. The top of the Great Caucasus under the name of Bazarduzu is considered the most south point Russia. She ascended to a height of 4466 meters above sea level. The first ascent to it was made in 1935.

You can talk about the mountains of Dagestan for a long time. But it has another unique attraction - just fifteen kilometers from Makhachkala, its capital, the gray-haired Caspian splashes - the largest closed reservoir on Earth, the largest drainless lake on the planet at the junction of Europe and Asia. Its area is 371 thousand square kilometers. The depth is more than a kilometer. It is home to more than 140 species of fish, of which the most famous is the beluga, which, if you meet, will get scared: is it really a shark?! There are sturgeons that produce black caviar and species such as bream, asp, bleak, river eel, spike, burbot - you can’t list them all! The great Russian river Volga, 3530 kilometers long, flows into the Caspian Sea (lake), off the coast of which a 300,000-strong Nazi army led by Field Marshal Paulus was taken prisoner near Stalingrad. Every year, thousands and thousands of tourists, both our compatriots and foreigners, come to rest to the Caspian Sea. In particular, there are sanatoriums, boarding houses, and children's health camps near Makhachkala. True, the shores of the Caspian have not yet been very well developed, but a course has been taken to create another popular resort area here. And what? White fine sand, clear water - sunbathe, swim, catch a fish, cook fragrant fish soup from it on the shore!

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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). 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 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). 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 is folded mountains with some volcanic activity that formed as the Alps in 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. (By comparison, Saudi Arabia, the country with the world's largest oil reserves, is estimated at 260 billion barrels.) From a geophysical point of view, the Caucasus forms a wide warp zone that is part of a 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. The Greater Caucasus is a grandiose folded mountainous region that occurred on 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, the highest mountain in 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 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 altitudes, 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.

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. All major rivers of the region begin here. The state border of Russia passes along it 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), highest point- 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 permanent ice is 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 latest research, 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 Azov seas. 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-clay sediments were deposited, in some troughs these deposits reached several kilometers. Gradually, several islands formed one big 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. The 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.


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