One of the brightest bodies of water in the world is Caspian lake, which is located at the junction of Asia and Europe, and its shores and waters belong to 5 countries. The Caspian Sea is attractive and inexpensive place for rest and treatment. Beautiful nature and the early opening of the swimming seasons make holidays on the Caspian coast more tempting.

The Caspian Lake is the largest of all lakes on the planet. It is often called the Caspian Sea because of its impressive dimensions and slightly salty water. It is located at the junction of Asia and Europe on the territory of 5 countries: Turkmenistan, Kazakhstan, Russian Federation Azerbaijan and Iran.

Despite the fact that the tourism infrastructure is inferior in level of development to the Black Sea, the Caspian coast is in demand among tourists. This is facilitated by the rapid warming of the reservoir due to its shallow depth; often the swimming season can begin at the end of April and end in October. The average water temperature in summer is 20-22 °C.

Advantages of holidays on the Caspian Lake:

• clean sea sand;
• picturesque nature;
• nautical healing climate;
• mineral springs;
• healing mud;
• the presence of sanatoriums of various orientations;
• excellent fishing, especially in Astrakhan;
• active entertainment for every taste (diving, rafting, windsurfing, etc.);
• low cost of housing and entertainment with developed infrastructure;
• being on the territory of the Russian Federation, which saves a lot of time on paperwork;
• great service;
• warm water for six months;
• the opportunity to save thousands of rubles on vacation, housing and food without denying yourself anything.

You can get to the Caspian Sea in different ways, but it’s worth deciding in the area of ​​which coastal city to plan your vacation.

In the Russian Federation on the Caspian Lake there are several resort towns:

Astrakhan is very popular among fishermen and amateurs active rest associated with water, because in its vicinity there are many rivers, and the Caspian Lake is just an hour away by car.

Ancient city Derbent also enjoys special love among tourists, because it is surrounded by such attractions as picturesque mountains, ancient fossils and legendary caves, overgrown with legends, and other interesting places to visit.

Such Dagestan resort cities as Izberbash, Kaspiysk, Makhachkala and Kalmyk Lagan are not deprived of attention. Many tourists come to the Caspian Lake and stay in Azerbaijani cities (Baku, Lankaran, Sumgait), Turkmen resorts Turkmentbashi and Avaza, Kazakh Aktau and Atyrau.

Origin of the Caspian Lake and its name

Over 5 million years ago, the ancient sea was divided into several smaller ones, including the Caspian and Black Sea. After this separation, the reservoirs repeatedly merged into one whole and were fragmented, but approximately 1.75-2 million years ago the reservoir was finally cut off from the waters of the World Ocean.

The modern name of the Caspian Lake is new. And according to one hypothesis, it came from the name of the Caspian tribe, who lived in its southwest in the first millennium BC.

Throughout the entire period of its existence, the Caspian Lake had more than 70 different names among various tribal peoples, including:

1. Abeskunskoye - after the name of the island and the city, which were located before their flooding by a reservoir in the 14th century in a low-lying plain formed by the Kura Kura River.
2. Saraiskoe.
3. Khazar or Mazandaran - an Iranian name in honor of the province of the same name of the country, located on the coast, is used in Iran to this day.
4. Dzhurdzhansky (Hirkansky) - the ancient Greek name of the reservoir, comes from the region of Hyrcania and the city of Gorgan, now belonging to Iran.
5. Derbentskoye is named after the ancient coastal town of the same name in Dagestan.
6. Sihai.
7. Khvaliyskoye is an ancient Russian name, derived from the name of the Khvalis people who lived in the north of the Caspian Sea.

Study and development of the Caspian Lake

Finds on the western coast of Dagestan indicate that people lived in this territory already 2 million ago. At the confluence of the river. Darvagchay (Dagestan) remains have been excavated at sites older than 600 thousand years. Excavations on the southern coast indicate human habitation in this area 75 thousand years ago. All these studies show that the climate and living conditions were suitable for humans.

The founder of geography and writer Hecataeus of Miletus (VI-V centuries BC) in his work “Description of the Earth” described the Caspian Sea as the Hyrcanian Sea. In the 5th century BC, the ancient Greek historian was one of the first to suggest that the Caspian is not connected with other seas or oceans, although scientists of those times argued that the reservoir was the northern bay of the World Ocean, which washed all known lands.

Aristotle in the 4th century BC was sure that the Hyrcanian reservoir was connected with the Black Sea by underground waters. Macedonsky studied the relationship of the Caspian Sea with other large bodies of water throughout his travels. In 323 BC, he sent the sailor and geographer Patroclus to explore the shores of the Caspian Sea.

The navigator reached the Kara-Bogaz Bay and considered it a river that connects the Caspian Lake with the ocean. The famous ancient Greek geographer and historian Strabo, in one of his 17 chronicles (books) “Geography”, represented the Caspian Lake stretched in the east-west direction.

Arab scientists of the 9th-13th centuries made a significant contribution to the study of the Caspian Sea, recording in their works information about coastal cities and states, islands, flowing rivers and oil that was produced in Azerbaijan (Baku).

The expansion of the geography of trade relations made it possible for European, Persian and Turkish travelers to receive a lot of information about the Caspian Sea. And the famous Marco Polo (XIII century) also described a huge reservoir.

A very detailed, although sometimes erroneous, map of the Caspian Sea was compiled in the 17th century by the famous scientist and traveler, the German Adam Olearius. Peter I repeatedly traveled towards the Caspian Lake, and based on the data he provided, Russian hydrographers compiled very detailed maps of the Caspian Sea.

Since the 17th century, exploration of the Caspian Sea and its coastal environs has become systematic and versatile. Peter the Great in 1714 sent a research expedition under the leadership of Bekovich-Cherkassky. A few years later, research was continued by Verdun and Soimonov, and a little later by Tokmachev, Voinovich and other scientists.

IN early XIX century, instrumental survey of the coast was carried out by I.F. Kolodkin, several decades later, geographical survey was carried out by an expedition led by N.A. Ivashintsev. For half a century, starting from 1866, regular hydrological and hydrobiological expeditions were carried out under the leadership of N.M. Knipovich.

During the first years of Soviet power, the Caspian Sea was actively explored by geologists, mainly in search of oil product deposits, studying the water balance and fluctuations in water height in the lake.

History of the Caspian Lake

The Caspian Lake is located on the site of one of the giant reservoirs of antiquity. The origin of the Caspian Lake is inextricably linked with the most ancient sea Tetris, which more than 50-55 million years ago united the Quiet and atlantic oceans, located on the territory of the present Caspian, Azov, Black and Mediterranean seas.

After long, complex tectonic movements, Tetris was first cut off from Pacific Ocean, and a little later the Atlantic.

About 5-6.5 million years ago, the giant reservoir broke into small basins, which included the Caspian and Black Sea.

After that, they repeatedly united and moved apart.

1.8-2 million years ago the Caspian Sea was finally cut off from the waters of the World Ocean and it was this time that is considered the beginning of its origin.

Throughout its history, the lake has changed its shoreline many times until it acquired its current appearance.

Physiographic characteristics of the Caspian Lake

The water surface of the lake is noticeably lower than the level of the World Ocean and amounts to -27.5...-28.5 m. The area of ​​the Caspian Sea varies depending on the level and water and is in the range of 380-390 km2, the total volume is 73.7-74.1 km3 .

The Caspian Sea is geographically divided into several parts with their own characteristics:

1. Northern Caspian— it accounts for 24% of the total area of ​​the reservoir. This part is small and its average depth does not exceed 6 m, the maximum reaches 25 m, the volume of water is less than 1%.
2. Middle Caspian– 36% of the total area of ​​the lake falls on it. This part of the lake is a kind of basin with a maximum depth of almost 800 m and an average depth of 190 m. It contains a third of the total volume of water.
3. Southern Caspian– occupies 40% of the total area of ​​the lake and accounts for the deepest part of the reservoir. It contains 2/3 of the volume of all water - 66%. The average depth is 340 m, and the deepest depression is 1025 m.

The length of the coastline reaches almost 7 thousand km. The maximum length of the lake is slightly more than 1 thousand km, and the widest point is 435 km. The minimum width is considered to be a segment of 195 km. The average width is considered to be 317 km.

Map of the depth of the Caspian lake

The shores vary greatly in their landscape. The northern coast is flat and low, around it there is semi-desert in the lowlands, and desert in the higher elevations. The southern coastline is partly lowland and partly mountainous and consists of the Elbrus ridge. The Caucasus Mountains come close to the western part.

The eastern coastline is a calcareous plateau of desert and semi-desert type. The outlines of the coast vary greatly depending on the water level, which fluctuates periodically.

Climate

The water temperature of the Caspian Sea fluctuates significantly depending on latitude. This amplitude is most noticeable in winter, when the water under the ice in the northern part has a temperature of 0.-0.5 °C above zero, while in the south at this time it is 10-11 °C.

According to average data, the temperature in the western part of the lake is up to 2 °C higher than in the eastern part, and when moving away from the shore it increases by 2-4 °C compared to the coastal zone. In summer, the water in the lake warms up to 23-29 °C, and in shallow water in the northern part it can reach 34-40 °C. Below 100 m, the temperature stabilizes at 4-7 °C.

The Caspian Lake is located three climatic zones: continental (north of the reservoir), temperate (middle) and subtropical (Southern Caspian). in winter average temperature ranges from -8 to -11 °C in the north and to +8 to +11 °C in the south of the lake.

In summer Northern part warms up to 24-25 °C with a positive mark; in the south the temperature rises to 26-27 °C. The highest temperature of +44 °C was recorded in the east of the reservoir.

The average annual precipitation is about 200 mm. Moreover, on the arid eastern coast at least 90-100 mm falls; in the southwest these figures can reach 1700 mm. The average annual wind speed is in the range of 3-8 m/s, mainly winds from the north prevail. In autumn and winter, their speed increases and can reach 35-39 m/s.

When the thermometer shows high sub-zero values ​​on the northern part of the lake, trees and flowers bloom on the southern coast. IN winter time The surface of the lake is unstable and stormy winds prevail. In winter, only the northern shallow waters freeze; during severe winter frosts, the Northern Caspian and the coastal waters of the Middle Caspian are covered with ice.

Flora and fauna

The flora of the Caspian Sea and its coastal environs consists of more than 720 plant species. The lake is mainly dominated by algae (diatoms, brown algae, etc.), and angiosperms - rupee and zoster. Most of the vegetation of the Caspian Lake originates from the Neogene period, but some entered the reservoir on the bottoms of ships or deliberately, with the help of humans.

Among the animal representatives of the Caspian Sea and its environs, there are more than 1,800 species, of which more than 400 are vertebrates, and more than 90 species are fish (sturgeon, carp, bream, mullet, beluga, etc.). Mammals are represented only by the Caspian seal, which is the smallest of the seal family and lives exclusively in the Caspian Lake.

The lake is home to the largest school of sturgeon in the world, and a lot of pike perch, carp and roach live in the sea waters. Up to 80% of the total world sturgeon catch and more than 90% of the world black caviar fishery come from the Caspian Lake.

The main migration route of birds between Europe and Asia passes over the Caspian Sea (in the spring - in the southern direction, and in the autumn - in the north). During seasonal migrations, over 11.5 million birds fly over the lake, about 5 million individuals remain for the winter. The lake itself is home to over 850 species of animals, of which almost 80 are vertebrates. More than 500 species of plants are present in the lake.

Islands

The Caspian Lake contains more than 50 large and medium-sized islands with a total area of ​​about 350 square meters. km.

State to which the island belongs	Island name
Azerbaijan	Jasper
	Oil Rocks
	pelicanium
	Zenbil
	Sengi Mugan
	Boyuk-Zira
	Baku archipelago
	Kichik Zira
	Kurinsky
	Chilov
	Ignat Dashi
	Inner Stone
	Khyarya Zira
	Kara Su
	Dash Zira
	Novoivanovsky
	Chikil
	Kurinskaya braid
	Gil
	Baburiy
Iran	Ashur-Ada
Kazakhstan	Seal Islands
	Average
	Südev
	Konevsky Oseredok
	Somyonok
	Babiy
	Somovy
Turkmenistan	Ogurchinsky
	Bolshoi Zyudostinsky
	Marine Ivan-Karul
	Clean Jars
	Maly Zyudostinsky
	little birdie
	Egg
	Maly Setnoy
	Jumpers
	Sandy
	Bazaar
	Konevsky
	Green
	Sea Privet
	Batkachny
	Nordic
	Maly Zhemchuzhny
	Big Setnoy
	Blinov
	Upper Oseredok
	Khokhlatsky
	Südev
	Lower
	Small
	Likhachev
	Seal
	Seventh
	Sea Chapura
	Chechen

Flowing rivers

More than 130 rivers flow into the Caspian Sea, 9 of which have a delta-shaped mouth. 95% of water enters the Caspian Sea from rivers. Most of them flow into the lake in the northern and western parts of the reservoir; there are no flowing rivers in the east.

The largest and most significant rivers of the Caspian basin:

Approximately 88% of the total flow comes from rivers such as the Volga, Terek, Ural and Emba, which flow into the northern Caspian Sea. 7% of the flow falls on rivers such as the Kura, Sulak, Samur and other smaller ones flowing into the western part of the Caspian Sea. About 5% of the flow of the Sefidrud, Kheraz and Gorgan rivers enters the Iranian part of the reservoir.

Ecological state

The condition of the Caspian Lake and surrounding areas causes concern among environmentalists.

Main causes environmental problems associated with a person and his activities:

• production and transportation of oil and gas products;
• influx of pollutants from river runoff waters;
• poaching;
• waste from coastal cities;
• rapid jumps in water levels in the Caspian Sea due to irrigation of lands with waters of inflowing rivers and the use of hydroelectric power stations.

How is the Caspian Lake used?

The Caspian Lake has been actively used by humans for many centuries.

Main directions economic activity:

Recreational resources of the Caspian Lake

The climate and nature of the Caspian coast with its clean sand beaches, healing mud and healing springs provide great potential and excellent conditions for sanatorium treatment and tourist recreation.

The development of the resort and tourism infrastructure, although noticeably inferior to the similar industry on the Black Sea coast, is actively expanding and the quality of service is improving. The most noticeable surge in development in recent years has been observed in the Republic of Dagestan, Iran, Turkmenistan and Azerbaijan.

Holidays on the Caspian coast in the Russian Federation and former countries The CIS is low in cost and on average the quality in some places is inferior to that in the Black Sea, but in actively developing places the level is quite high.

Popular recreation areas with developed infrastructure:

• Baku;
• Amburan;
• Makhachkala;
• Bilgah;
• Derbent.
• Nabran;
• Lankaran;
• Nardaran.

The development of the Turkmen resort and tourism industry is hampered by internal policies that isolate the state from the majority of tourists. And in Iran, mass recreation is difficult due to strict Sharia laws.

There are 3 protected areas on the coast:

The Caspian Lake is located at the junction of Europe and Asia and is the largest lake in the world.

There are many interesting facts about the reservoir:

1. Its size is larger than Japan, but its area is smaller than Germany.
2. In terms of depth, the Caspian Sea is in third place, second only to Tanganyika and Baikal.
3. Every 2.5 centuries the waters are completely renewed.
4. Albino beluga sturgeon, whose caviar is the most expensive in the world, is caught on the Iranian coast. It is distinguished by a white tint and is packaged in unusual jars made of real gold.
5. The largest beluga weighed more than 1200 kg and was caught in the 20s. XX century on the Russian coast. In its dimensions it is comparable to a large shark.
6. Throughout the history of the lake, it has had more than 70 different names.
7. Scientists are still debating whether to consider the Caspian Lake a sea, arguing that its area exceeds the size of some seas, and the bottom is created according to the oceanic type. But at the same time, the reservoir is endorheic and is not connected to the ocean or other seas.
8. The smallest coastline of the five countries belongs to the Russian Federation.
9. More than 80% of the water enters the lake from the river. Volga.

The Caspian Lake is rich in flora and fauna, distinguished by warm waters and a long swimming season. It is best known for its depth and size, production of oil, gas and sturgeon, the reserves of which exceed those known throughout the world.

The lake is 95% supplied with runoff water from rivers. On its coast there are many resorts and sanatoriums, whose attractiveness can be assessed by affordable prices.

Article format: Mila Friedan

Video about the Caspian Sea

Film about the Caspian Sea:

The Caspian Sea is one of the largest salty bodies of water on Earth, located at the junction of Europe and Asia. His total area is about 370 thousand sq. km. The reservoir receives more than 100 water streams. The largest rivers flowing into the Volga, Ural, Emba, Terek, Sulak, Samur, Kura, Atrek, Sefidrud.

The Volga River - the pearl of Russia

The Volga is a river flowing on the territory of the Russian Federation, partially crossing Kazakhstan. It belongs to the category of the largest and longest rivers on Earth. Total length The Volga is more than 3500 km. The river originates in the village of Volgoverkhovye, Tver Region, located on After that, it continues its movement through the territory of the Russian Federation.

It flows into the Caspian Sea, but does not have direct access to the World Ocean, so it is classified as internal drainage. The watercourse receives about 200 tributaries and has more than 150 thousand outlets. Today, reservoirs have been built on the river to regulate flow, which has sharply reduced fluctuations in water levels.

The river's fisheries are varied. In the Volga region, melon growing predominates: the fields are occupied by grain and industrial crops; table salt is extracted. Oil and gas deposits have been discovered in the Urals region. The Volga is the largest river flowing into the Caspian Sea, so it is of great importance for Russia. The main transport structure that allows you to cross this stream is the longest in Russia.

Ural - river in Eastern Europe

The Ural, like the Volga River, flows on the territory of two states - Kazakhstan and the Russian Federation. Historical name - Yaik. It originates in Bashkortostan at the top of the Uraltau ridge. The Ural River flows into the Caspian Sea. Its pool is the sixth largest in the Russian Federation, and its area is more than 230 square meters. km. Interesting fact: The Ural River, contrary to popular belief, belongs to an inland European river, and only its upper course in Russia belongs to Asia.

The mouth of the watercourse gradually becomes shallow. At this point the river divides into several branches. This feature is characteristic along the entire length of the channel. During floods, you can observe how the Ural overflows its banks, in principle, like many other Russian rivers flowing into the Caspian Sea. This is especially observed in places with a gently sloping coastline. Flooding occurs at a distance of up to 7 meters from the riverbed.

Emba - river of Kazakhstan

Emba is a river flowing in the territory of the Republic of Kazakhstan. The name comes from the Turkmen language, literally translated as “valley of food”. The river basin has an area of ​​40 thousand square meters. km. The river begins its journey in the Mugodzhary mountains and, as it flows, it gets lost among the swamps. When asking which rivers flow into the Caspian Sea, we can say that in high-flow years the Emba reaches its basin.

Along the river's coastline, natural resources such as oil and gas are being extracted. The issue of passing the border between Europe and Asia along the Emba watercourse, as in the case of the river. Ural, an open topic even today. The reason for this is a natural factor: the mountains of the Ural Range, which are the main landmark for drawing boundaries, disappear, forming a homogeneous terrain.

Terek - mountain water stream

Terek is a river of the North Caucasus. The name is literally translated from Turkic as “poplar”. The Terek flows from the glacier of Mount Zilga-Khokh, located in the Trusovsky Gorge of the Caucasus Range. passes through the lands of many states: North Ossetia, Georgia, Stavropol Territory, Kabardino-Balkaria, Dagestan and the Chechen Republic. It flows into the Caspian Sea and Arkhangelsk Bay. The length of the river is just over 600 km, the basin area is about 43 thousand square meters. km. An interesting fact is that every 60-70 years the flow forms a new transit branch, while the old one loses its strength and disappears.

The Terek, like other rivers flowing into the Caspian Sea, is widely used to satisfy human economic needs: it is used to irrigate the arid areas of the adjacent lowlands. There are also several hydroelectric power stations located on the water stream, the total average annual production of which is more than 200 million kWh. New additional stations are planned to be launched in the near future.

Sulak - water stream of Dagestan

Sulak is a river connecting the Avar Koisu and Andean Koisu streams. It flows through the territory of Dagestan. It begins in the Main Sulak Canyon and ends its journey in the waters of the Caspian Sea. The main purpose of the river is to supply water to two cities of Dagestan - Makhachkala and Kaspiysk. Also, several hydroelectric power stations are already located on the river, and new ones are planned to be launched to increase the generated power.

Samur - the pearl of Southern Dagestan

Samur is the second largest river in Dagestan. The name is literally translated from Indo-Aryan as “abundance of water.” It originates at the foot of Mount Guton; It flows into the waters of the Caspian Sea through two branches - Samur and Small Samur. The total length of the river is just over 200 km.

All rivers flowing into the Caspian Sea are of great importance for the territories through which they flow. Samur is no exception. The main purpose of using the river is to irrigate land and provide residents of nearby cities with drinking water. It is because of this that the waterworks and a number of the Samur-Divichi canal were built.

At the beginning of the twentieth century (2010), Russia and Azerbaijan signed an interstate agreement requiring both parties to rationally use the resources of the Samur River. The same agreement introduced territorial changes between these countries. The border of the two states has been moved to the middle of the hydroelectric complex.

Kura - the largest river in Transcaucasia

When wondering which rivers flow into the Caspian Sea, I would like to describe the Kuru stream. It flows on the land of three states at once: Turkey, Georgia, Azerbaijan. The length of the stream is more than 1000 km, the total area of ​​the basin is about 200 thousand square meters. km. Part of the basin is located on the territory of Armenia and Iran. The source of the river is in the Turkish province of Kars, flowing into the waters of the Caspian Sea. The path of the river is thorny, laid among hollows and gorges, for which it received its name, which translated from the Mingrelian language means “gnaw”, that is, the Kura is a river that “gnaws” itself among the mountains.

There are many cities on it, such as Borjomi, Tbilisi, Mtskheta and others. It plays an important role in meeting the economic needs of the residents of these cities: hydroelectric power stations are being built, and the Mingachevir reservoir created on the river is one of the main fresh water reserves for Azerbaijan. Unfortunately, the ecological state of the stream leaves much to be desired: the level of harmful substances is several times higher than the permissible limits.

Features of the Atrek River

Atrek is a river located on the territory of Iran and Turkmenistan. It originates in the Turkmen-Kharasan mountains. Due to active use for economic needs for irrigation, the river has become shallow. For this reason, it reaches the Caspian Sea only during flood periods.

Sefidrud - high-water river of the Caspian Sea

Sefidrud is a major river of the Iranian state. Initially it was formed by the confluence of two water streams - Kyzyluzen and Shahrud. Now it flows out of the Shabanau reservoir and flows into the depths of the Caspian Sea. The total length of the river is more than 700 km. The creation of a reservoir became a necessity. It made it possible to minimize the risk of flooding, thereby protecting the cities located in the river delta. The waters are used to irrigate lands with a total area of ​​more than 200 thousand hectares of land.

As can be seen from the presented material, the Earth's water resources are in unsatisfactory condition. The rivers flowing into the Caspian Sea are actively used by people to satisfy their needs. And this has a detrimental effect on their condition: watercourses are depleted and polluted. That is why scientists around the world are sounding the alarm and conducting active propaganda, calling for saving and conserving water on Earth.

CASPIAN SEA (Caspian), the largest enclosed body of water on the globe, an endorheic brackish lake. Located on the southern border of Asia and Europe, it washes the shores of Russia, Kazakhstan, Turkmenistan, Iran and Azerbaijan. Due to the size, originality natural conditions and the complexity of hydrological processes, the Caspian Sea is usually classified as a closed inland sea.

The Caspian Sea is located in a vast area of ​​internal drainage and occupies a deep tectonic depression. The water level in the sea is about 27 m below the level of the World Ocean, the area is about 390 thousand km 2, the volume is about 78 thousand km 3. The greatest depth is 1025 m. With a width of 200 to 400 km, the sea extends along the meridian for 1030 km.

The largest bays: in the east - Mangyshlaksky, Kara-Bogaz-Gol, Turkmenbashi (Krasnovodsky), Turkmensky; in the west - Kizlyarsky, Agrakhansky, Kizilagaj, Baku Bay; in the south there are shallow lagoons. There are many islands in the Caspian Sea, but almost all of them are small, with a total area of ​​less than 2 thousand km 2. In the northern part there are numerous small islands adjacent to the Volga delta; larger ones are Kulaly, Morskoy, Tyuleniy, Chechen. Off the western shores are the Absheron archipelago, to the south lie the islands of the Baku archipelago, east coast- a narrow island, stretched from north to south, Ogurchinsky.

The northern shores of the Caspian Sea are low-lying and very sloping, characterized by the widespread development of drying areas formed as a result of surge phenomena; deltaic shores are also developed here (deltas of the Volga, Ural, Terek) with an abundant supply of terrigenous material; the Volga delta with extensive reed thickets stands out. The western shores are abrasive, south of the Absheron Peninsula, mostly accumulative deltaic type with numerous bay bars and spits. The southern shores are low. The eastern shores are mostly deserted and low-lying, composed of sand.

Relief and geological structure bottom.

The Caspian Sea is located in a zone of increased seismic activity. In the city of Krasnovodsk (now Turkmenbashi) in 1895, a powerful earthquake measuring 8.2 on the Richter scale occurred. On the islands and coast of the southern part of the sea, eruptions of mud volcanoes are often observed, leading to the formation of new shoals, banks and small islands, which are eroded by waves and appear again.

Based on the peculiarities of physical-geographical conditions and the nature of the bottom topography in the Caspian Sea, it is customary to distinguish the Northern, Middle and Southern Caspian Seas. The Northern Caspian Sea is distinguished by exceptionally shallow waters, located entirely within the shelf with average depths of 4-5 m. Even small changes in the level here on low-lying coasts lead to significant fluctuations in the area of ​​the water surface, therefore the boundaries of the sea in the north-eastern part are shown with a dotted line on small-scale maps. The greatest depths (about 20 m) are observed only near the conventional border with the Middle Caspian, which is drawn along a line connecting the island of Chechen (north of the Agrakhan Peninsula) with Cape Tyub-Karagan on the Mangyshlak Peninsula. The Derbent depression (maximum depth 788 m) stands out in the bottom topography of the Middle Caspian Sea. The border between the Middle and Southern Caspian Sea passes over the Absheron threshold with depths of up to 180 m along a line from Chilov Island (east of the Absheron Peninsula) to Cape Kuuli (Turkmenistan). The Southern Caspian basin is the most extensive area of ​​the sea with the greatest depths; almost 2/3 of the waters of the Caspian Sea are concentrated here, 1/3 is in the Middle Caspian, and less than 1% of the Caspian waters are located in the Northern Caspian due to shallow depths. In general, the topography of the Caspian Sea bottom is dominated by shelf areas (the entire northern part and a wide strip along the eastern coast of the sea). The continental slope is most pronounced on the western slope of the Derbent Basin and almost along the entire perimeter of the South Caspian Basin. On the shelf, terrigenous-shelly sands, shell, and oolitic sands are common; deep-sea areas of the bottom are covered with siltstone and silty sediments with a high content of calcium carbonate. In some areas of the bottom, bedrock of Neogene age is exposed. Mirabilite accumulates in the Kara-Bogaz-Gol Bay.

Tectonically, within the Northern Caspian Sea, the southern part of the Caspian syneclise of the Eastern European Platform is distinguished, which in the south is framed by the Astrakhan-Aktobe zone, composed of Devonian-Lower Permian carbonate rocks that lie on a volcanic base and contain large deposits of oil and natural combustible gas. From the southwest, Paleozoic folded formations of the Donetsk-Caspian zone (or Karpinsky ridge) are thrust onto the syneclise, which is a protrusion of the foundation of the young Scythian (in the west) and Turanian (in the east) platforms, which are separated at the bottom of the Caspian Sea by the Agrakhan-Guryev fault (left shear) of northeastern strike. The Middle Caspian mainly belongs to the Turanian platform, and its southwestern margin (including the Derbent depression) is a continuation of the Terek-Caspian foredeep of the Greater Caucasus fold system. The sedimentary cover of the platform and trough, composed of Jurassic and younger sediments, contains deposits of oil and combustible gas in local uplifts. The Absheron threshold, separating the Middle Caspian from the South, is a connecting link of the Cenozoic folded systems of the Greater Caucasus and Kopetdag. The South Caspian basin of the Caspian Sea with crust of oceanic or transitional type is filled with a thick (over 25 km) complex of Cenozoic sediments. Numerous large hydrocarbon deposits are concentrated in the South Caspian Basin.

Until the end of the Miocene, the Caspian Sea was a marginal sea of ​​the ancient Tethys Ocean (from the Oligocene - the relict oceanic basin of the Paratethys). By the beginning of the Pliocene, it lost contact with the Black Sea. The Northern and Middle Caspian Seas were drained, and the paleo-Volga valley stretched through them, the delta of which was located in the Absheron Peninsula region. Delta sediments have become the main reservoir of oil and natural combustible gas deposits in Azerbaijan and Turkmenistan. In the late Pliocene, in connection with the Akchagyl transgression, the area of ​​the Caspian Sea greatly increased and the connection with the World Ocean was temporarily resumed. The waters of the sea covered not only the bottom of the modern depression of the Caspian Sea, but also the adjacent territories. In Quaternary time, transgressions (Apsheron, Baku, Khazar, Khvalyn) alternated with regressions. The southern half of the Caspian Sea is located in a zone of increased seismic activity.

Climate. The Caspian Sea, strongly elongated from north to south, is located within several climatic zones. In the northern part the climate is temperate continental, on the west coast it is warm temperate, southwestern and south coast lie within the subtropics; the east coast is dominated by a desert climate. In winter, over the Northern and Middle Caspian, the weather is formed under the influence of Arctic continental and sea air, and the Southern Caspian is often under the influence of southern cyclones. The weather in the west is unstable and rainy, in the east it is dry. In summer, the western and northwestern regions are influenced by the spurs of the Azores atmospheric maximum, and the southeastern ones are influenced by the Iran-Afghan minimum, which together creates dry, stable warm weather. Over the sea, winds prevail in the northern and northwestern (up to 40%) and southeastern (about 35%) directions. average speed winds are about 6 m/s, in the central regions of the sea up to 7 m/s, in the area of ​​the Absheron Peninsula - 8-9 m/s. Northern storm “Baku Nords” reach speeds of 20-25 m/s. The lowest average monthly air temperatures -10 °C are observed in January - February in the northeastern regions (in the most severe winters they reach -30 °C), in southern regions 8-12 °C. In July - August, average monthly temperatures over the entire sea area are 25-26 °C, with a maximum of 44 °C on the east coast. The distribution of atmospheric precipitation is very uneven - from 100 mm per year on the eastern shores to 1700 mm in Lankaran. The open sea receives an average of about 200 mm of precipitation per year.

Hydrological regime. Changes in the water balance of an enclosed sea greatly influence changes in the volume of water and corresponding fluctuations in level. Average long-term components of the water balance of the Caspian Sea for the 1900-90s (km 3 /cm layer): river runoff 300/77, precipitation 77/20, underground runoff 4/1, evaporation 377/97, ​​runoff to Kara-Bogaz- Gol 13/3, which forms a negative water balance of 9 km 3, or 3 cm of layer, per year. According to paleogeographic data, over the past 2000 years, the range of fluctuations in the level of the Caspian Sea has reached at least 7 m. Since the beginning of the 20th century, level fluctuations have shown a steady downward trend, as a result of which over 75 years the level dropped by 3.2 m and in 1977 reached -29 m (lowest position in the last 500 years). The sea surface area has decreased by more than 40 thousand km 2, which exceeds the area of ​​the Sea of ​​Azov. Since 1978, a rapid rise in level began, and by 1996 a mark of about -27 m relative to the level of the World Ocean was reached. In the modern era, fluctuations in the level of the Caspian Sea are determined mainly by fluctuations in climatic characteristics. Seasonal fluctuations in the level of the Caspian Sea are associated with the unevenness of river flow (primarily the Volga runoff), therefore the lowest level is observed in winter, the highest in summer. Short-term sharp changes in level are associated with surge phenomena; they are most pronounced in shallow northern areas and during storm surges can reach 3-4 m. Such surges cause flooding of large coastal areas of land. In the Middle and Southern Caspian Sea, surge fluctuations in level average 10-30 cm, under storm conditions - up to 1.5 m. The frequency of surges, depending on the region, is from one to 5 times a month, lasting up to one day. In the Caspian Sea, as in any closed body of water, seiche level fluctuations are observed in the form of standing waves with periods of 4-9 hours (wind) and 12 hours (tidal). The magnitude of seiche vibrations usually does not exceed 20-30 cm.

River flow in the Caspian Sea is distributed extremely unevenly. More than 130 rivers flow into the sea, which on average bring about 290 km 3 of fresh water per year. Up to 85% of the river flow falls on the Volga and the Urals and enters the shallow Northern Caspian Sea. The rivers of the western coast - Kura, Samur, Sulak, Terek, etc. - provide up to 10% of the flow. About 5% more fresh water brought to the South Caspian by rivers of the Iranian coast. The eastern desert shores are completely deprived of constant fresh flow.

The average speed of wind currents is 15-20 cm/s, the highest - up to 70 cm/s. In the Northern Caspian Sea, the prevailing winds create a flow directed along the northwestern coast to the southwest. In the Middle Caspian, this current merges with the western branch of the local cyclonic circulation and continues to move along the western coast. Near the Absheron Peninsula the current bifurcates. Its part in the open sea flows into the cyclonic circulation of the Middle Caspian, and the coastal part goes around the shores of the Southern Caspian and turns north, joining the coastal current that goes around the entire eastern coast. The average state of movement of Caspian surface waters is often disturbed due to variability in wind conditions and other factors. Thus, in the northeastern shallow area, a local anticyclonic gyre may arise. Two anticyclonic eddies are often observed in the Southern Caspian Sea. In the Middle Caspian in the warm season, stable northwest winds create southerly transport along the eastern coast. In light winds and during calm weather currents may have other directions.

Wind waves develop very strongly, since the prevailing winds have a long acceleration length. The disturbance develops mainly in the northwest and southeast directions. Strong storms are observed in the open waters of the Middle Caspian Sea, in the areas of Makhachkala, the Absheron Peninsula and the Mangyshlak Peninsula. The average wave height of greatest frequency is 1-1.5 m; at wind speeds of more than 15 m/s it increases to 2-3 m. The highest wave heights are recorded during strong storms in the area of ​​the Neftyanye Kamni hydrometeorological station: annually 7-8 m, in some cases up to 10 m.

The water temperature on the sea surface in January - February in the Northern Caspian Sea is close to freezing temperature (about -0.2 - -0.3 °C) and gradually increases southward to 11 °C off the coast of Iran. In summer, surface waters warm up to 23-28 °C everywhere, except for the eastern shelf of the Middle Caspian Sea, where in July - August seasonal coastal upwelling develops and the surface water temperature drops to 12-17 °C. In winter, due to intense convective mixing, the water temperature changes little with depth. In summer, under the upper heated layer at horizons of 20-30 m, a seasonal thermocline (a layer of sharp temperature changes) is formed, separating deep cold waters from warm surface ones. In the bottom layers of water in deep-sea depressions, the temperature remains 4.5-5.5 °C all year round in the Middle Caspian and 5.8-6.5 °C in the Southern Caspian. Salinity in the Caspian Sea is almost 3 times lower than in open areas of the World Ocean, averaging 12.8-12.9‰. It should be especially emphasized that the salt composition of Caspian water is not completely identical to the composition ocean waters, which is explained by the isolation of the sea from the ocean. The waters of the Caspian Sea are poorer in sodium salts and chlorides, but richer in carbonates and sulfates of calcium and magnesium due to the unique composition of salts entering the sea with river and underground runoff. The highest salinity variability is observed in the Northern Caspian, where in the estuarine areas of the Volga and Ural the water is fresh (less than 1‰), and as we move south, the salt content increases to 10-11‰ at the border with the Middle Caspian. The greatest horizontal salinity gradients are characteristic of the frontal zone between sea and river waters. The differences in salinity between the Middle and Southern Caspian Seas are small; salinity increases slightly from northwest to southeast, reaching 13.6‰ in the Turkmen Gulf (in Kara-Bogaz-Gol up to 300‰). Vertical changes in salinity are small and rarely exceed 0.3‰, which indicates good vertical mixing of waters. Water transparency varies widely from 0.2 m in the mouth areas of large rivers to 15-17 m in the central regions of the sea.

According to the ice regime, the Caspian Sea is classified as a partially frozen sea. Ice conditions are observed annually only in the northern regions. The Northern Caspian is completely covered by sea ice, the Middle Caspian is partially covered (only in severe winters). Middle border sea ​​ice runs along an arc convex to the north, from the Agrakhan Peninsula in the west to the Tyub-Karagan Peninsula in the east. Ice formation usually begins in mid-November in the extreme northeast and gradually spreads to the southwest. In January, the entire Northern Caspian Sea is covered with ice, mostly fast ice (immobile). Drifting ice borders the fast ice with a strip 20-30 km wide. The average ice thickness is from 30 cm at the southern border to 60 cm in the northeastern regions of the Northern Caspian Sea, in hummocky accumulations - up to 1.5 m. The destruction of the ice cover begins in the 2nd half of February. In severe winters, drifting ice is carried south, along the western coast, sometimes to the Absheron Peninsula. At the beginning of April, the sea is completely free of ice cover.

History of the study. It is believed that modern name The Caspian Sea comes from the ancient Caspian tribes who inhabited the coastal regions in the 1st millennium BC; other historical names: Hyrkan (Irkan), Persian, Khazar, Khvalyn (Khvalis), Khorezm, Derbent. The first mention of the existence of the Caspian Sea dates back to the 5th century BC. Herodotus was one of the first to claim that this body of water is isolated, that is, it is a lake. In the works of Arab scientists of the Middle Ages there is information that in the 13th-16th centuries the Amu Darya partially flowed into this sea through one of its branches. The well-known numerous ancient Greek, Arabic, European, including Russian, maps of the Caspian Sea until the beginning of the 18th century did not reflect reality and were actually arbitrary drawings. By order of Tsar Peter I, in 1714-15, an expedition was organized under the leadership of A. Bekovich-Cherkassky, who explored the Caspian Sea, in particular its eastern shores. The first map, on which the contours of the coasts are close to modern ones, was compiled in 1720 using astronomical definitions by Russian military hydrographers F.I. Soimonov and K. Verdun. In 1731, Soimonov published the first atlas, and soon the first printed sailing guide of the Caspian Sea. A new edition of maps of the Caspian Sea with corrections and additions was carried out by Admiral A.I. Nagaev in 1760. The first information on the geology and biology of the Caspian Sea was published by S. G. Gmelin and P. S. Pallas. Hydrographic research in the 2nd half of the 18th century was continued by I.V. Tokmachev, M.I. Voinovich, and at the beginning of the 19th century by A.E. Kolodkin, who for the first time carried out instrumental compass surveying of the coast. Published in 1807 new map Caspian Sea, compiled taking into account the latest inventories. In 1837, systematic instrumental observations of sea level fluctuations began in Baku. The first was completed in 1847 Full description Gulf of Kara-Bogaz-Gol. In 1878, a General Map of the Caspian Sea was published, which reflected the results of the latest astronomical observations, hydrographic surveys and depth measurements. In 1866, 1904, 1912-13, 1914-15, under the leadership of N. M. Knipovich, expeditionary research was carried out on the hydrology and hydrobiology of the Caspian Sea; in 1934, the Commission for the Comprehensive Study of the Caspian Sea was created at the USSR Academy of Sciences. A great contribution to the study of the geological structure and oil content of the Absheron Peninsula and the geological history of the Caspian Sea was made by Soviet geologists I. M. Gubkin, D. V. and V. D. Golubyatnikovs, P. A. Pravoslavlev, V. P. Baturin, S. A Kovalevsky; in the study of water balance and sea level fluctuations - B. A. Appolov, V. V. Valedinsky, K. P. Voskresensky, L.S. Berg. After the Great Patriotic War, systematic, comprehensive research was launched in the Caspian Sea, aimed at studying the hydrometeorological regime, biological conditions and geological structure of the sea.

In the 21st century in Russia, two large scientific centers are engaged in solving the problems of the Caspian Sea. The Caspian Marine Research Center (CaspMNRC), created in 1995 by decree of the Government of the Russian Federation, conducts research work in hydrometeorology, oceanography and ecology. The Caspian Research Institute of Fisheries (CaspNIRKH) traces its history back to the Astrakhan Research Station [established in 1897, since 1930 the Volga-Caspian Scientific Fisheries Station, since 1948 the Caspian Branch of the All-Russian Research Institute of Fisheries and Oceanography, since 1954 the Caspian Scientific Research Institute of Marine Fisheries and Oceanography (CaspNIRO), modern name since 1965]. CaspNIRH is developing the foundations for the conservation and rational use of biological resources of the Caspian Sea. It consists of 18 laboratories and scientific departments - in Astrakhan, Volgograd and Makhachkala. It has a scientific fleet of more than 20 vessels.

Economic use. Natural resources The Caspian Sea is rich and varied. Significant hydrocarbon reserves are being actively developed by Russian, Kazakh, Azerbaijani and Turkmen oil and gas companies. There are huge reserves of mineral self-sedimented salts in the Kara-Bogaz-Gol Bay. The Caspian region is also known as a massive habitat for waterfowl and semi-aquatic birds. About 6 million migratory birds migrate across the Caspian Sea every year. In this regard, the Volga delta, Kyzylagaj, Northern Cheleken and Turkmenbashi bays are recognized as sites of international rank within the framework of the Ramsar Convention. The mouth areas of many rivers flowing into the sea have unique types of vegetation. The fauna of the Caspian Sea is represented by 1800 species of animals, of which 415 are vertebrate species. More than 100 species of fish live in the sea and river mouths. Marine species are of commercial importance - herring, sprat, gobies, sturgeon; freshwater - carp, perch; Arctic “invaders” - salmon, white fish. Large ports: Astrakhan, Makhachkala in Russia; Aktau, Atyrau in Kazakhstan; Turkmenbashi in Turkmenistan; Bender-Torkemen, Bender-Anzeli in Iran; Baku in Azerbaijan.

Ecological state. The Caspian Sea is under powerful anthropogenic influence due to the intensive development of hydrocarbon deposits and the active development of fishing. In the 1980s, the Caspian Sea provided up to 80% of the world's sturgeon catch. Predatory fishing in recent decades, poaching and a sharp deterioration of the environmental situation have brought many valuable fish species to the brink of extinction. The living conditions of not only fish, but also birds and sea animals (Caspian seal) have deteriorated. Countries washed by the waters of the Caspian Sea are faced with the problem of creating a set of international measures to prevent pollution of the aquatic environment and developing the most effective environmental strategy for the near future. A stable ecological state is observed only in parts of the sea remote from the coast.

Lit.: Caspian Sea. M., 1969; Comprehensive studies of the Caspian Sea. M., 1970. Issue. 1; Gul K.K., Lappalainen T.N., Polushkin V.A. Caspian Sea. M., 1970; Zalogin B.S., Kosarev A.N. Seas. M., 1999; International tectonic map of the Caspian Sea and its frame / Ed. V. E. Khain, N. A. Bogdanov. M., 2003; Zonn I. S. Caspian Encyclopedia. M., 2004.

M. G. Deev; V. E. Khain (geological structure of the bottom).

The Caspian Sea is simultaneously considered both an endorheic lake and a full-fledged sea. The reasons for this confusion are brackish waters and hydrological regime, similar to the sea.

The Caspian Sea is located on the border of Asia and Europe. Its area is about 370 thousand km 2, its maximum depth is just over one kilometer. The Caspian Sea is conventionally divided into three almost equal parts: Southern (39% of the area), Middle (36%) and Northern (25%).

The sea washes simultaneously the Russian, Kazakh, Azerbaijani, Turkmen and Iranian shores.

Shore of the Caspian Sea(Caspian Sea) has a length of approximately 7 thousand kilometers, if you count it together with the islands. In the north, the low seashore is covered with swamps and thickets, and has multiple water channels. The eastern and western coasts of the Caspian Sea have a winding shape; in some places the shores are covered with limestone.

There are many islands in the Caspian Sea: Dash-Zira, Kur Dashi, Dzhambaisky, Boyuk-Zira, Gum, Chigil, Here-Zira, Zenbil, Ogurchinsky, Tyuleniy, Ashur-Ada, etc. Peninsulas: Mangyshlak, Tyub-Karagan, Absheron and Miankale. Their total area is approximately 400 km 2.

Flows into the Caspian Sea more than a hundred different rivers, the most significant are the Ural, Terek, Volga, Atrek, Emba, Samur. Almost all of them provide 85–95% of the annual water flow to the sea.

The largest bays of the Caspian Sea: Kaydak, Agrakhansky, Kazakh, Dead Kultuk, Turkmenbashi, Mangyshlaksky, Gyzlar, Girkan, Kaydak.

Climate of the Caspian Sea

The Caspian Sea is located in three climatic zones: subtropical climate in the south, continental in the north and temperate in the middle. In winter, the average temperature varies from -10 to +10 degrees, while in summer the air warms up to about +25 degrees. During the year, precipitation ranges from 110 mm in the east to 1500 mm in the west.

The average wind speed is 3–7 m/s, but in autumn and winter it often increases to 35 m/s. The most windy areas are the coastal areas of Makhachkala, Derbent and the Absheron Peninsula.

Water temperature in the Caspian Sea ranges from zero to +10 degrees in winter, and from 23 to 28 degrees in the summer months. In some coastal shallow waters the water can warm up to 35-40 degrees.

Only the northern part of the sea is subject to freezing, but in especially cold winters the coastal zones of the middle part are added to it. Ice cover appears in November and disappears only in March.

Problems of the Caspian region

Water pollution is one of the main environmental problems of the Caspian Sea. Oil production, various harmful substances from flowing rivers, waste from nearby cities - all this negatively affects the condition of sea water. Additional troubles are created by poachers, whose actions reduce the number of fish of certain species found in the Caspian Sea.

Rising sea levels are also causing serious financial harm to all Caspian countries.

According to conservative estimates, restoring destroyed buildings and taking comprehensive measures to protect the coast from flooding costs tens of millions of dollars.

Cities and resorts on the Caspian Sea

The most big city and the port washed by the waters of the Caspian Sea is Baku. Among the others settlements Azerbaijan, located in close proximity to the sea, are Sumgait and Lankaran. On the eastern shores is the city of Turkmenbashi, and about ten kilometers from it by the sea is the large Turkmen resort of Avaza.

On the Russian side, on the seashore there are the following cities: Makhachkala, Izberbash, Derbent, Lagan and Kaspiysk. Astrakhan is often called a port city, although it is located approximately 65 kilometers from the northern shores of the Caspian Sea.

Astrakhan

There are no beach holidays in this region: along the sea coast there are only continuous reed thickets. However, tourists go to Astrakhan not for lounging on the beach, but for fishing and various types active recreation: diving, catamaran riding, jet skiing, etc. In July and August, excursion ships ply along the Caspian Sea.

Dagestan

For a classic seaside holiday, it’s better to go to Makhachkala, Kaspiysk or Izberbash - that’s where not only good sandy beaches, but also decent recreation centers. The range of entertainment on the seashore on the Dagestan side is quite wide: swimming, healing mud springs, windsurfing, kiting, rock climbing and paragliding.

The only disadvantage of this direction is the underdeveloped infrastructure.

In addition, among some Russian tourists there is an opinion that Dagestan is far from the most peaceful territory that is part of the North Caucasus Federal District.

Kazakhstan

A much calmer environment can be found in the Kazakh resorts of Kuryk, Atyrau and Aktau. The last one is the most popular tourist city Kazakhstan: there are many good entertainment venues and well-maintained beaches. In summer it's very heat, reaching up to +40 degrees during the daytime, and dropping only to +30 at night.

Disadvantages of Kazakhstan tourist country— the same poor infrastructure and rudimentary transport links between regions.

Azerbaijan

The most the best places Baku, Nabran, Lankaran and other Azerbaijani resorts are considered for holidays on the Caspian coast. Fortunately, everything is fine with the infrastructure in this country: for example, several modern comfortable hotels with swimming pools and beaches have been built in the Absheron Peninsula area.

However, in order to enjoy a holiday on the Caspian Sea in Azerbaijan, you need to spend a lot of money. In addition, you can only get to Baku quickly enough by plane - trains rarely run, and the journey from Russia itself takes two to three days.

Tourists should not forget that Dagestan and Azerbaijan are Islamic countries, so all “non-believers” need to adapt their usual behavior to local customs.

Subject to simple rules nothing will spoil your holiday on the Caspian Sea.

The territory of Russia is washed by twelve seas belonging to the basins of three oceans. But one of these seas - the Caspian - is often called a lake, which sometimes confuses people who have little understanding of geography.

Meanwhile, it is really more correct to call the Caspian a lake rather than a sea. Why? Let's figure it out.

A little geography. Where is the Caspian Sea located?

Occupying an area that exceeds 370,000 square kilometers, the Caspian Sea stretches from north to south, dividing the spaces of Europe and Asia with its water surface. Its coastline belongs to five different countries: Russia, Kazakhstan, Azerbaijan, Turkmenistan and Iran. Geographers conventionally divide its water area into three parts: the Northern (25% of the area), the Middle (36% of the area) and the Southern Caspian (39% of the area), which differ in climate, geological conditions and natural features. The coastline is predominantly flat, indented by river channels, covered with vegetation, and in the northern part, where the Volga flows into the Caspian Sea, it is also swampy.

The Caspian Sea has about 50 large and small islands, about one and a half dozen bays and six large peninsulas. In addition to the Volga, approximately 130 rivers flow into it, and nine rivers form fairly wide and branched deltas. The annual drainage of the Volga is about 120 cubic kilometers. Shared with others large rivers– Terek, Ural, Emba and Sulak – this accounts for up to 90% of the total annual runoff into the Caspian Sea.

Why is the Caspian called a lake?

The main feature of any sea is the presence of straits connecting it to the ocean. The Caspian Sea is a closed or drainless body of water that receives river water, but is not connected to any ocean.


Its water contains a very small amount of salt compared to other seas (about 0.05%) and is considered slightly salty. Due to the absence of at least one strait connecting to the ocean, the Caspian Sea is often called the largest lake in the world, since the lake is a completely enclosed body of water that is fed only by river water.

The waters of the Caspian Sea are not subject to international maritime laws, and its waters are divided between all countries that are adjacent to it, in proportion to the coastline.

Why is the Caspian called a sea?

Despite all of the above, most often in geography, as well as in international and internal documents, the name “Caspian Sea” is used, and not “Caspian Lake”. First of all, this is explained by the size of the reservoir, which is much more characteristic of the sea than of the lake. Even, which is much smaller in area than the Caspian Sea, is often called a sea by local residents. There are no other lakes in the world whose shores belong simultaneously to five different countries.

In addition, you should pay attention to the structure of the bottom, which near the Caspian Sea has a pronounced oceanic type. Once upon a time, the Caspian Sea most likely connected with the Mediterranean, but tectonic processes and drying out separated it from the World Ocean. There are more than fifty islands in the Caspian Sea, and the area of ​​some of them is quite large, even by international standards they are considered large. All this allows us to call the Caspian a sea, and not a lake.

origin of name

Why is this sea (or lake) called the Caspian? The origin of any name is often associated with ancient history terrain. Different peoples who lived on the shores of the Caspian called it differently. More than seventy names of this reservoir have been preserved in history - it was called the Hyrcanian, Derbent, Sarai Sea, etc.


Iranians and Azerbaijanis still call it the Khazar Sea. It began to be called Caspian after the name of the ancient tribe of nomadic horse breeders who lived in the steppes adjacent to its coast - the numerous Caspian tribe. It was they who gave the name to the largest lake on our planet - the Caspian Sea.