The Caspian lowland is located in Eurasia. This is the southern tip of the East European Plain, adjacent to the Caspian Sea in its northern part. Natural boundaries: from the north - the General Syrt upland, to the west - the Volga, Stavropol uplands and Ergeni, to the east - the Pre-Ural plateau and Ustyurt, from the south - the Caspian Sea. Located on the territory of Russia and Kazakhstan.

Coordinates:
Latitude: 47°32"N
Longitude: 49°01"E

The Caspian lowland is a huge plain with an area of ​​200,000 sq. km, falling below sea level from the south. These are steppes, deserts, semi-deserts and salt marshes, although many rivers flow there, including large ones: the Volga, at its confluence with the Caspian Sea, forming a vast delta, and the Ural. Emba, Terek, Kuma cross the lowland. There are many salt lakes - Baskunchak, Inder, Aralsor, Kamys-Samar lakes, Elton, Botkul.

Among the pancake-flat plains, here and there rise domes of salt called mountains. Big Bogdo, a 150-meter-high salt mountain, is a cult place for Buddhists. The main part of the lowland is steppes and sands used for pastures. In the Volga-Ural interfluve, fishing and hunting are developed; the famous Astrakhan watermelons grow in the Volga floodplain. There are oil and gas fields in the Ural-Emba interfluve.

IN Caspian lowland, despite the seeming sparsity of nature, there are many natural attractions. There are archaeological, historical, cultural different peoples and eras.

Russia

Nature reserves “Bogodino-Baskunchaksky”, “Astrakhansky”, “Black Lands”. “Volga-Akhtubinskaya floodplain” is a natural park. Nature reserves “Manych-Gudilo” and “Sands of Burley”, Mount Bolshoye Bogdo, Lotus Valley, Kuma-Manych depression (separates Eurasia), Kordon tract, Baer hillocks. Archeological monuments: Devil's ancient settlement of the Golden Horde era (Astrakhan region), Sarai-Batu (Astrakhan region), burials in Turtles of the Bronze Age, "Samosdelka" settlement (Astrakhan region). Among the cultural sites, one can note the Khosheutovsky khurul (Kalmyk monument in honor of the victory over Napoleon in the village of Rechnoye, Astrakhan region), the watermelon museum (the city of Kamyzyak).

Kazakhstan

Ustyurt Nature Reserve, Karagiye depression on the Mangyshlak peninsula, Lake Shalkar (Aktobe region), floodplain forests of the Ural River with unique and relict vegetation, Sanal and Sazanbay canyons. On the Caspian coast there is the resort town of Aktau and the Kenderli complex. You can travel along the Great Silk Road, which passed through these places. There are many archaeological sites: Kyzyl-Kala (red fortress), the city of Sary-Aichik - the Golden Horde trade center. The sacred places of Muslims are the underground mosques of Shopan-Ata and Beket-Ata.

The Caspian Lowland is located in the southeastern part of the Russian Plain, adjacent to the Caspian Sea. In the west, the lowland is bordered by the eastern slopes of the Stavropol plateau and Ergeni, in the north by the slopes of General Syrt. In the east, the border coincides with the Pre-Ural plateau and the Northern Chink of the Ustyurt plateau. In the southern part, significant areas lie below sea level by 27m.

Most of the lowland is administratively part of the Kazakh SSR - the West Kazakhstan Territory and partly in the regions of the Volgograd, Saratov, Astrakhan and Kalmyk Autonomous Soviet Socialist Republics.

The Caspian lowland is located within a deep tectonic basin - the Caspian syneclise, founded in the Paleozoic and representing a complex and heterogeneous section of the Russian Platform. The syneclise is complicated by a number of tectonic structures IIorder. Crystalline rocks lie here at a depth of more than 3000 m and are overlain by Paleozoic and Meso-Cenozoic sediments. Within the lowlands, Permian deposits of Kungurian age are developed from ancient rocks, at the base of which lie rock salt stocks. The Permian rocks are overlain by Triassic sediments. They are overlain by Jurassic, Cretaceous and Paleogene sediments. The end of the Paleogene is characterized by orogenic movements that covered large areas. They are associated with the lowering of the lowland and the penetration of seas into its territory. The most extensive was the Akchagyl basin, which occupied almost the entire territory of the modern Caspian Sea, the Caspian Lowland and penetrated to the north. Long sleeve This basin also went towards the Black Sea. In the north, the sediments of this basin are represented by thin, thick-layered clays, and near the coast - by sands; In some places there are small layers of oil shale. The total thickness of Akchagyl deposits reaches 80-100 m. The Absheron basin, which replaced the Akchagyl basin, was smaller. He left sands, conglomerates, clays with a thickness of more than 400 m. Quaternary deposits are represented by genera of marine and continental origin with a thickness of over 30 m. Marine sediments consist of clayey, sandy-clayey and sandy strata with marine fauna left by the Baku, Khozar, Lower and Upper Khvalynsk transgressions. They alternate with continental deposits - loess-like loams, sands, peat bogs, silts.

The deposits of the Lower Khvalynsk transgression are represented by chocolate clays and partly loams. The southern part was subject to the Upper Khvalynian transgression. The consequence of the Upper Khvalynian transgression are sands and sandy loams of the Upper Khvalynian age. The boundary between the two indicated transgressions runs approximately along the zero horizontal line.

Many researchers synchronize the Caspian transgressions with the glaciation periods of the Russian Plain, but due to insufficient data, the synchronization scheme is not yet sufficiently substantiated.

The Caspian lowland is characterized by peculiar structures - salt domes, characteristic of salt tectonics. The reason for their formation is associated with orogenic movements, due to which horizontally lying layers of Permian, Mesozoic and Tertiary rocks in many places are folded into small brachyanticlinal folds containing a gypsum and salt core.

Due to tangential pressure, salt masses were squeezed upward from the original deposit and broke through the overlying rocks, forming domes. Due to the redistribution of salt masses, new places of their concentration were created. Salt domes are hills 100-150 m high. m, in which gypsum and salts come to the surface (M. Bogdo, B. Bogdo, Bis-Chokho, Chapchagi, etc.). Associated with them is the existence of self-sedating lakes - Elton, Baskunchak, etc., which are fed by saline solutions coming from salt domes. In the Emba region, oil fields are also confined to domes composed of Jurassic and Lower Cretaceous rocks.

Orographically, the Caspian Lowland is a large depression, flat, gently inclined towards the sea. M.V. Karandeeva writes that the main type of lowland relief is the marine accumulative plain. Erosion, aeolian, suffosion and other types and forms of relief are developed on it.

The northern part of the Caspian lowland is characterized by monochromatic flat surfaces, the relative heights of which do not exceed 1.0-1.5 m. The sea flat plains are broken by depressions and numerous hillocks - marmots. Depressions are depressions with a depth of 0.3 to 2.0 m and diameter from 10 to 100 m. Their shape is usually round or oval. They stand out on the surface of the lowland not so much because of their depth as because of their fresher and greener vegetation.

Among the flat sea plains in this part of the lowland, erosional landforms are developed, which are presented in the form of hollows. The hollows sometimes stretch for tens of kilometers, in several rows. They begin in the northern part of the lowland and end in the estuaries, before reaching the Caspian Sea. Small hollows usually do not have clearly defined slopes, their width is 100 - 1000 m. An example of hollows is the Sarpinsko-Davanskaya, which stretches from Krasnoarmeysk to the south, along Ergeni, and then breaks up into branches. The hollow is covered with a thin layer of alluvium; in the Ergeni region it is currently covered with alluvium from ravines, which divides the hollow into separate depressions - lakes. The formation of hollows is associated with the flows of the receding sea. The Sarpinsko-Davanskaya hollow once served as a branch of the Volga and was fed by its waters. After the Volga deepened its channel, the Sarpinsko-Davanskaya hollow was separated from it, and its further existence occurred due to temporary flows from Ergeni. In addition to the above-described landforms, coastal landforms have been preserved within the lowland: estuaries, takyrs, etc., which are confined to the boundaries of the distribution of the Khvalyn seas.

Due to the fact that in the southern part of the lowland large areas are occupied by sand, aeolian relief prevails here. Between the Volga and Ergeni, as well as to the east on the Volga-Ural watershed, there are massifs of blowing sands - Astrakhan and Ryn-Sands. Here the sands form in places dunes 5-6 high m, and sometimes 15 m, mounds, ridges and basins. The basins have a depth of up to 8 m, and area - up to 3 km 2. Their shape is in most cases oval; the windward slopes are steep and the leeward slopes are gentle. Sand blown from the basins is deposited in the form of mounds on the surfaces adjacent to their western and northwestern sides.

Along the shores of the Caspian Sea, from the river. Emba to the mouth of the river. Kuma, there are mounds elongated almost in the latitudinal direction, the so-called Baer mounds. Their height is 7 - 10 m, width - 200-300 m and length - from 0.5 to 8 km. The width of interridge depressions reaches 400-500 m. During floods of the Volga they are filled with water. The city of Astrakhan and all the villages within the Volga delta are built on these hillocks.

There is still no consensus on the origin of the mounds. Academician K. M. Baer assumed that they occurred from a catastrophically rapid flow of water during a sudden drop in the level of the Caspian Sea. I.V. Mushketov explains the origin of the mounds for various reasons: some mounds were formed due to the dislocation of the main rocks on which Caspian sediments were deposited (near Kamennoy Yar), others are a product of erosion (near Astrakhan), and others are overgrown valleys (near Enotavka). B. A. Fedorovich explains the origin of the Baer mounds by the corrosive and accumulative activity of the wind, the predominant direction of which coincides with the Voeikov axis, oriented latitude-wise in the northern Caspian region.

Salt domes, the Volga-Akhtuba and Ural valleys add variety to the lowland relief. The Volga Valley is a blooming oasis against the background of a semi-desert. The islands in the river's floodplain are green with groves of sedges, silver poplars, and willows. The Volga Valley within the lowland is incised by 20-30 m into the Lower and Upper Khvalynian marine sediments, which serve as the bedrock coast. The right bank is steep, vertical, and is strongly washed away by the river. The left main bank is located at a great distance from the riverbed. On the left bank there is a well-developed floodplain terrace (Volga-Akhtubinskaya), which extends for tens of kilometers.

The hydrographic network of the lowland is poor; Three large transit rivers flow within its boundaries: the Volga, Ural and Terek, which have no tributaries within the lowland. Rivers drain only the narrow coastal strips immediately adjacent to them. In addition to these rivers, there are several small rivers - Bolshoy and MaliyUzen, Uil, Sagiz, Kushum, which dry up in the hot season or break up into separate

closed, more or less significant basins of standing water, forming lake spills. An example is the Sarpinsky lakes, which collect water flowing from the Ergeniy, in the central part - the Kamysh-Samarsky lakes, receiving the waters of the Bolshoi and Maly Uzeni, and others. The waters of the river. In dry years, the Kums do not reach the Caspian Sea, and the waters of the river. The embs reach it only during high water. In summer in the river The Embe, like all small rivers of the semi-desert, has brackish water. Within the lowlands there are a lot of small and large salt and occasionally fresh lakes. Fresh lakes arise in depressions closed on all sides, in which melted snow waters collect.

The climate of the Caspian Lowland is characterized by the greatest continentality compared to other regions of the Russian Plain. This is due to the distance from Atlantic Ocean, with a predominance of continental air masses and increased insolation.

In winter, the spread of the spurs of the Siberian anticyclone and the associated cold eastern winds, the frequency of which reaches 50%, play a significant role in the formation of weather conditions. Temperatures in the winter months in the Caspian region are unusually low for this latitude (from -14 in the north to -8° on the Caspian Sea coast). The same temperature conditions are observed in winter in Arkhangelsk and Leningrad. In some cases, frosts reach -30, -40°. The Caspian Sea, which freezes in the northern part, does not have a warming effect even on coastal areas. Snow cover lasts 4-5 months, but its height is small - 10-20cm.

Spring in the Caspian region is friendly and short - during the end of April and beginning of May, the temperature rises rapidly due to increased incoming radiation and the influx of warm air from the southern regions of Kazakhstan.

Summer is very hot and dry. The amount of total solar radiation for June-August reaches 50 kcal/cm 2, the same amount as in Crimea. Isotherms of the summer months are located in the latitudinal direction: in the northern part of the Caspian region the average July temperature is about +22°, in the southern part +23, +24°. The absolute maximum temperature is above +40°.

Maximum precipitation falls in the first half of summer, most often in the form of short-term showers, and is only 20-30 mm per month. Annual precipitation amounts decrease in the southeast direction from 350 to 200-150 mm. Evaporation is about 1000 mm, thus, the total moisture deficit reaches 800mm.

Droughts, characteristic of the southern and southeastern regions of the European territory of the USSR, are here of the greatest intensity and frequency (up to 30%). Dry winds blow very often, especially dry and hot ones, over the sandy semi-deserts of the southeast.

The Caspian lowland lies in the semi-desert zone, and is characterized by light chestnut solonetzic soils, the absorbent complex of which contains sodium. Thickness of humus horizons - 30-40 cm, the amount of humus is small in the upper horizons - 1-3%, and it is distributed unevenly across the soil profile. The lower part of the soil profile is saline with soluble salts. The soil cover of the semi-desert is variegated: it consists of light chestnut solonetzic soils, solonetzes and leached meadow-chestnut soils of depressions. The semi-desert is characterized by an abundance of salt lakes, salt marshes and rivers carrying salt water. Salt marshes stretch along the shores of the Caspian in a wide strip. Sands are widespread in the Astrakhan Trans-Volga region. A significant part of these sand massifs belongs to the moving category.

In the north of the Caspian lowland, the vegetation is represented by the wormwood-cereal type; As you move south, the number of grasses decreases and wormwood begins to predominate. In the south, saltworts predominate. The grass cover here is very sparse, the vegetation is low-growing, due to which it suffers less from evaporation: the plants have a very highly developed root system, allowing them to intensively use soil moisture. On slightly saline loams, the predominant importance is: white wormwood( Artemisia maritima), and on clayey, more saline soils - black wormwood ( Artemisia pauciflora); a lot of fescue ( Festuca sulcata), feather grass( Stipa capillata), thin-legged ( Koeleria gracilis). There are many tulips in spring( Tulipa schrenkii), buttercup ( Ranunculus polyrhisus), bluegrass (Roa bulbosa var vivipara). On salt licks, in addition to black wormwood, biyurgun solyanka grows ( Anabasis salsa) and lichens ( Aspicilia); in rainy times, colonies of algae appear on the salt licks, looking like black, hair-like threads pressed to the ground, more than 30 in lengthcm.

Various saltworts, black wormwood and shrubs grow on the salt marshes: tamarisk ( Tamarix romosissima), kermek ( Statice suffruticosa). Kiyak grass grows on the sands( Elymus giganteus), which is a sand fixer. In wet hollows among the sands there are willows( Salix rosmarinifolia), sucker ( Elaeagnus angustifolia) and other shrubs. In the depressions, among the lumpy sands, where fresh groundwater lies very close to the surface, white poplar grows( Populus alba), sedge (Ro Pulus nigra), aspen, willow ( Salix rosmarinifOla), rose hip ( Rosa cinnamomea). In the Volga floodplain there are: oak( Quercus robur), elm ( Ulmuslaevis), sedge

Characteristic representatives of animals are: sandy or yellow gopher( Citellus fulvus), jerboa ( Alactaga elates), gerbil ( Meriones tamariscinus), hamster ( Cricetus cricetus). Saiga is found in the sands between the Volga and the Urals( Saiga tatarica), Corsac fox is widespread( Vulpes corsac).

Among the birds found: black lark( Melanocorypha yeltonieusis) and small ( Calandrella). The floodplains and deltas of rivers, especially the Volga, abound in birds. Typical for the Volga delta: great cormorant( Phalacrocorax carbo), white-tailed eagle( Haliaetus albicilla), grey goose (Apse rapseg), egret ( Egretta alba), Sultan's chicken( Porphyrio polioeephalus), pheasant ( Phasianus colchicus), mustachioed tit ( Ponurus biarmicus).

The Caspian lowland is used as pasture. The low depth of snow cover allows the use of pastures in winter. With estuary irrigation, it is possible to obtain high yields of wheat, millet and forage grasses.

In the Volga-Akhtuba floodplain, melon growing, horticulture and gardening, sowing industrial crops and rice flourish.

In the Astrakhan Nature Reserve there is a relict plant - lotus( Nelumbium caspicum).

The Emba oil field is being developed and table salt is being extracted (Lake Baskunchak and Elton).

- Source-

Davydova, M.I. Physical geography of the USSR / M.I. Davydova [and others]. – M.: Education, 1966.- 847 p.

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The Caspian Lowland is located on the territory of Kazakhstan and Russia. It got its name due to its geographical location: the plain occupies the northern part of the largest salt lake in the world - the Caspian Sea.

general characteristics

The Caspian Lowland is a plain inclined at a slight angle to the Caspian Sea. It extends 500 km from north to south, 700 km from west to east, and covers an area of ​​about 200 thousand square meters. km.

The height above sea level of the Caspian lowland varies: the highest point of the northern regions is 149 m, and the southern regions are located 28 m below sea level. On the territory of the plain there are minor elevations: Big and Small Bogdo, Inder Mountains and others.

Rice. 1. Caspian Sea.

The boundaries of the Caspian lowland are:

• in the north - the Caspian Sea;
• in the southeast - the Russian Plain;
• in the west - Kazakhstan.

In the northwest of the lowland there is an area called the Black Lands. It is a semi-desert area that is not covered with snow even in winter due to strong winds. These lands got their name from the dark brown soils and black wormwood.

The territory of the plain consists of several powerful tectonic structures: the Caspian deep depression, the Ergeninskaya Upland, the Terek and Nogai depressions. Many years ago the plain was regularly flooded by the sea. As a result, loams were formed in the north, and sandy deposits in the south.

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The plain is crossed by such water arteries like the Ural, Volga, Terek, Emba, Sulak, Kuma. With the arrival of the summer heat, low-water rivers dry up or branch into lake floods. This region is also rich in salt lakes, including Inder, Baskunchak, Botkul, Elton and others.

The Caspian lowland belongs to Russian Federation(Astrakhan region, Kalmykia, Dagestan) and Kazakhstan. The largest cities in this territory are Aty Rau (Kazakhstan) and Astrakhan (RF).

Rice. 2. Astrakhan.

Features of climate and nature

The Caspian lowland is characterized by a very dry climate. In winter, strong cold winds blow, the air temperature drops to -10-15C, not too much snow falls, but it does not linger on the surface due to windy weather.

Summer for this area is hot, with very meager precipitation. Not uncommon dust storms and dry winds that form sand hills - dunes.

Rice. 3. Nature of the Caspian lowland.

The soil on the plain is highly saline and has many shades, from dark brown to light chestnut. In the north, steppes predominate, in the southern regions of the lowlands - deserts and semi-deserts.

Not all plants are able to withstand such harsh conditions, and in these parts only cereals and wormwood are widespread. 1/5 of the total area is allocated for arable land, where melons are traditionally grown.

The fauna of the Caspian lowland is also not very diverse. Marmots, ferrets, and water rats live here. The most valuable animal is the seal. The sturgeon fishery is well developed.

What have we learned?

When studying the topic “Caspian Lowland,” we learned how the Caspian Lowland was formed, what its area, structural features, and boundaries are. We learned what climate, animals and vegetable world characteristic of this plain.

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The famous Black Lands reserve, created in a place where there are practically no people living and no water, is located in the Caspian lowland, a most interesting object from the point of view of science and geotourism. The Caspian Lowland is a territory located at the extreme point of the southeast of the Russian Plain and encircling the Caspian Sea. In the southeast, the black lands or Khar-Gazr in Kalmyk, approaches the Volga delta, this is where another interesting natural object- Baer mounds (in honor of Ak.

Where is the Caspian lowland located on the physical map?

K.M. Burr, who discovered this miracle of nature), which are sand ridges up to 45 meters high and up to 300 meters wide, the length of which is several kilometers. Between the hillocks you can see ilmens, small lakes overgrown with grass; any activity is prohibited here, as it can destroy these delightful creations of nature.

On the territory of the Caspian lowland there is the Volga-Akhtuba floodplain, where the Great Russian River, dividing into many branches, there are about 800 of them, flows into the Caspian Sea and ends its course. A natural park of the same name was established in this territory with the aim of protecting the ecosystem and nests of more than 200 species of birds. This place is extremely popular among fishermen, because the variety and size of underwater inhabitants can surprise even the most experienced fisherman! Therefore, when traveling in the Volga Delta, you should definitely take a selfie with a huge catch, especially since fishing promotions in July will allow you to save significantly on this type of vacation. Another miracle of nature located in the Caspian lowland can be safely called the famous salt lake Baskunchak, which is rightfully considered a bottomless bowl of salt. In addition to the above-mentioned attractions created by nature, it should also be noted: the Lotus Valley, the Burley Sands reserve, the Kordon tract, the Manych-Gudilo nature reserve and, of course, the Big Bogdo salt dome.

In addition to natural attractions, the region is also rich in historical ones. Among the architectural monuments, it is worth noting such as the Devil's Settlement, located in the Ikryaninsky district, erected during the time of the Golden Horde, Sarai-Batu, or as it is also called Selitrennoye Gordische, is a fortified complex built around the beginning of the 13th century. It is also worth noting the burials discovered here, dating back to Bronze Age and more recent monuments, such as the Khosheutovsky khurul, a monument to the wars that defeated Napoleon. Also on the territory of cities located in the Caspian lowland there are many cultural and religious buildings built in different eras.

The largest city located here is Astrakhan, the center of the region of the same name; most of the enterprises involved in the extraction and processing of minerals, which are rich in the lowland area, are concentrated here. And oil, uranium, gas, and many industrial and precious metals are mined here.
Part of the Caspian lowland is located on the territory of Kazakhstan; here the largest regional center is the city of Atyrau, considered the oil capital of all of Kazakhstan.

The Caspian lowland is not only the “Black Land” where nothing grows except wormwood, but also the most fertile lands of the Astrakhan region, where the climate allows you to grow some of the most delicious watermelons. The list of attractions in the region is not limited to the list above; even ten similar articles would not be enough to describe them all; such a volume of printed information is unlikely to be adequately absorbed, therefore, if you are interested, we advise you to visit this unique place located on the territory of our Motherland. Good luck.

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The relief of the Saratov region is diverse; in one article we cannot show you how different it is from each other different parts area, so we will write about each type of relief separately. In this article you will learn everything about the Caspian Lowland, including its geological structure and hydrography. Read the article about the geological structure of the Saratov region in our article: Geological structure of the Saratov region.

Caspian lowland is located in the basin of the lower reaches of the Bolshoy and Maly Uzenya rivers and occupies the southeastern part of the Saratov region.

Caspian Lowland: description and features

Geologically, this lowland is the youngest - it is a marine accumulative plain of early Khvalynian age. Its surface is smooth, slightly hilly and slightly dissected. Absolute elevations: in the north - from 45-50 m, in the south - 20-25 m. Flat, featureless watersheds up to 50 m high are composed of sea sands, sandy loams and “chocolate” clays of early Khvalynian age, lying almost horizontally.

On its surface there are many estuaries, as well as small “steppe saucers” (depressions) with a diameter of 1.5-2 m. Some estuaries form lakes and wetlands due to the accumulation of melt water.

The relief of the region is characterized by modern movement of the earth's crust. It is accompanied by increased erosion processes (growth of ravines, landslides, sinkholes, etc.) and leveling of the relief. Also read our article about the Relief of the Saratov region.

The lowland is separated from the Syrtovaya Plain to the north by a well-defined abrasive pre-Syrtove ledge, which has the shape of a straight slope 50-80 m wide, less often 20 m. The surface of the plain has a slight slope to the south and southeast.

Estuaries, suffoeic depressions, saucer-shaped depressions, mounds of biogenic origin, coastal ramparts, lakes, differing in shape, size, and duration of the waterway, are widespread. The river and ravine-gully network on it is poorly developed. The lowland is composed of clays, loams, and sands. The depth of valley incision does not exceed 2-5 m. Erosion gives way to accumulation.

Caspian lowland in quaternary period was the scene of several Caspian transgressions. The largest of them was the early Prague, when the sea covered the entire lowland. The boundary of this transgression in the north is clearly marked by an abrasion scarp. Since then, erosion and other processes have little changed the original appearance of the sea plain.

The Caspian lowland is confined to the Caspian syneclise and is currently an area of ​​subsidence and accumulation of a thick (up to 17 km) cover of sedimentary deposits. Against the background of the general subsidence, areas of intense uplift stand out in places where salt domes and massifs develop.

When writing the article, the following sources were used: Geography of the Saratov region. Saratov, 1997, sargidro.narod.ru; Photo: 5klass.net

Sights of Russia: Caspian Lowland

Abstract on the topic:

Caspian lowland

Plan:

Introduction
• 1Geographical location
• 2Geological structure
• 3Climate and vegetation
• 4Economic significance
• 5Source

Introduction

Caspian lowland- a lowland located on the East European Plain, surrounding the northern part of the Caspian Sea.

1. Geographical location

The Caspian lowland is bordered in the north by General Syrt, in the west by the Volga Upland and Ergeni, in the east by the Pre-Ural Plateau and Ustyurt. The area of ​​the lowland is about 200 thousand km². The height above sea level is up to 149m, the southern part of the lowland lies below sea level (up to −28m).

The Caspian lowland is a flat surface, gently inclined towards the sea, among which rise individual hills - the Inder Mountains, Big Bogdo, Small Bogdo and others.

The Caspian lowland is crossed by the rivers Ural, Volga, Terek, Kuma and others. Small rivers (Bolshoy and Maly Uzen, Wil, Sagiz) dry up in the summer or break up into a number of basins, forming lake spills - Kamysh-Samara lakes, Sarpinsky lakes. There are many salt lakes (Baskunchak, Elton, etc.).

2. Geological structure

The Caspian lowland includes several large tectonic structures (Caspian syneclise, Ergeninsky uplift, Nogai and Tersk depressions). In Quaternary times, the lowland was repeatedly flooded by the sea, which left clayey and loamy deposits in the northern part and sandy deposits in the southern part.

The surface of the Caspian lowland is characterized by micro- and mesoforms in the form of depressions, estuaries, spits, hollows, in the south - eolian forms, and along the coast of the Caspian Sea - a strip of Baer hillocks.

3. Climate and vegetation

The climate is sharply continental. Average temperatures in January range from −14° in the north to −8° on the coast; in July, respectively, +22°, +23°. Precipitation ranges from 200-150mm in the southeast to 350mm in the northwest, evaporation is about 1000mm. Dry winds are frequent.

The soils and vegetation of the Caspian lowland are characterized by great complexity. Salt licks and solonchaks are often found.

In the north there are wormwood-grass steppes on light chestnut soils, in the south there are semi-deserts and deserts on brown and sandy soils with a predominance of wormwood.

4.

Map of the Caspian lowland

Economic significance

Used as pasture.

In the Volga-Akhtuba floodplain, melon growing, gardening, and vegetable growing are widespread.

Oil and gas production (Caspian oil and gas province), in lakes - extraction of table salt (lakes Baskunchak, Elton, etc.).

5. Source

Grigoriev A.A. Brief geographical encyclopedia. Volume 3. - M.: Soviet Encyclopedia, 1962. - P.580.

Satellite photograph of the lower Volga, Caspian Lowland and northern Caspian Sea

Caspian lowland- lowland surrounding the northern part of the Caspian Sea.

Geographical position

The Caspian lowland is bordered in the north by the Common Syrt, in the west by the Volga Upland and Ergeni, in the east by the Pre-Ural plateau and Ustyurt. The area is about 200 thousand km². The height is up to 149m, the southern part of the lowland lies below ocean level and is −28m.

The Caspian lowland is crossed by the rivers Ural, Volga, Terek, Kuma; small rivers(B. and M. Uzen, Wil, Sagiz) dry up in the summer or disintegrate into a number of basins, forming lake spills - Kamysh-Samara lakes, Sarpinsky lakes. There are many salt lakes (Baskunchak, Elton, etc.).

The Caspian lowland is a flat surface, gently inclined towards the sea, among which rise individual hills - the Inderskpe Mountains, Big Bogdo, Small Bogdo and others.

Map on Google.Earth

Geological structure

The Caspian lowland includes several large tectonic structures (Caspian syneclise, Ergeninsky uplift, Nogai and Tersk depressions). In Quaternary times it was repeatedly flooded by the sea, which left clay and loamy deposits in the northern part and sandy deposits in the southern part.

The surface of the Caspian lowland is characterized by micro- and mesoforms in the form of depressions, estuaries, spits, hollows, in the south - aeolian forms, and along the coast of the Caspian Sea - a strip of Baer hillocks.

Climatic conditions

The climate is dry, continental.

Caspian lowland

Average temperatures in January range from −14° in the north to −8° on the coast; in July, respectively, +22°, +23°. Precipitation ranges from 200-150mm in the southeast to 350mm in the northwest, evaporation is about 1000mm. Dry winds are frequent.

The soils and vegetation of the Caspian lowland are characterized by great complexity. The soils are light chestnut, solonetzic, and there are solonetzes and solonchaks. In the north there is wormwood-cereal vegetation, to the south the number of cereals decreases, and wormwood begins to predominate. Used as pasture. In the Volga-Akhtuba floodplain there is melon growing, horticulture, and vegetable growing. Oil fields (Emben oil region), table salt in lakes (Baskunchak, Elton lakes, etc.).

Source

Grigoriev A.A. Volume 3 // Concise geographical encyclopedia. - M.: Soviet Encyclopedia, 1962. - P. 580 p.

§ 24. Plains (textbook)

§ 24. Plains

1.Remember how plains are indicated on the map.

2.What landforms are common in your area?

Surface of plains. Our planet is dominated by flat terrain. This is clearly visible on the physical map of the hemispheres.

There are plains flat. The surface is smooth, there are no noticeable ascents and descents. Eat rolling plains, Where increases alternate with decreases. However, such inequalities have a relative height of no more than 200 m. Therefore, plains- These are relatively flat areas of the earth's surface with slight fluctuations in height. Most of the plains of the globe are huge in size. Their names reflect this: Great Chinese Plain in Eurasia, Great Plains in North America. On one Eastern European Plain The territory of many states fit in - Ukraine, Belarus, Moldova, Lithuania, Latvia, Estonia and Russia (western part).

Heights of the plains. Based on the altitude above sea level, the plains are divided into low (lowlands), high (highlands) and high (Plateau).

Lowlands have absolute heights of up to 200 m.

For example, West Siberian Plain with a flat surface in Eurasia. On the earth's surface there are lowlands located even below sea level. For example, Caspian lowland lies 28 m below sea level.

Hills— These are plains with absolute heights from 200 to 500 m. Hills include, for example Podolsk in Ukraine.

Plateau— These are also plains, only they are quite high - more than 500 m above sea level. Examples are Central Siberian Plateau and plateaus Dean in Asia.

The flat terrain of Ukraine is created by alternating lowlands and hills. By physical map It is easy to determine where they are located: the yellowish color of the hills differs from the green color indicating the lowlands. So, Pridneprovskayaelevation located in the western part, and Black Sea Lowland lies in the south of the country. However, in nature it is difficult to notice the transition from one type of plain to another. If you travel, for example, from Odessa to Vinnitsa, then the terrain will gradually rise and the traveler, unnoticed by himself, will continue his journey no longer on the lowlands, but on the hills. Changes in absolute altitudes can only be determined using special instruments.

Education of the plains. Plains can form as a result of the seabed being raised and freed from water. This is observed during vertical movements of the earth's crust. Such plains are called primary. For example, Prichernomorskayalowland was once a section of the bottom of the Black Sea.

Secondaryplains are formed in different ways. Some of them, created by river sediments (sands, loams), accumulated for a long time in depressions of the earth's crust. Their surface is flat or slightly wavy. So, Mesopotamian lowland formed by sediments of the Tigris and Euphrates rivers. Plains can also arise in place of mountains when, under the influence of external processes, their peaks and slopes are destroyed, and basins are filled with debris. Then the mountainous terrain gradually levels out and turns into a hilly plain. An example is Kazakh small hills— A high plain, among which rise individual remnants of mountain ranges. Ukraine is such a plain Donetsk Ridge.

Plains are usually covered with thick sedimentary rocks: sand, clay, forests, gravel, limestone. Deep beneath them lie igneous and metamorphic rocks: granite and gneiss. In some places they come to the surface. Layers of sedimentary rocks lie horizontally or with a slight slope. You can determine in which direction the plain is tilted both on the ground and on the map by the direction of the rivers.

Changes in the surface of the plains. Plains change under the influence of internal and external processes. Plains, as a rule, lie on platforms - ancient, leveled, stable sections of lithospheric plates. Therefore, internal processes manifest themselves there mainly in slow vertical movements.

External processes are associated with the work of water and wind. Where there is enough flowing water, river valleys and ravines are formed. Ravines destroy areas of fertile land. To combat them, people plant bushes and trees. In deserts where it is dry, the surface of the plains changes due to weathering, as well as the action of the wind, which creates sand ridges, dunes and dunes. Nowadays, human economic activity has also become a significant external force. During the construction of cities and roads, ravines are filled up and embankments are created. When mining minerals, quarries appear, and hills of waste rock grow near the mines - waste heaps Unfortunately, human transformation of a natural surface often has negative consequences. Careless economic activity can lead to the emergence of a dense network of ravines, turning fertile lands into wastelands.

Questions and tasks

1.What are called plains? What kind of surface can plains have?

2.How are plains differentiated by height?

3. Using the height scale in the atlas, determine what color each type of plain is indicated by height. Give examples of each type of plain.

4.What kind of plains are there in Ukraine?

5. The Dnieper divides Ukraine into Right Bank and Left Bank. Using the physical map of Ukraine, determine which one is higher.

6.How are plains formed?

7. Under the influence of what processes can the surface of the plains change?

General characteristics of the Caspian lowland

The northern coast of the Caspian Sea is occupied by a lowland of the same name. Part of this lowland is located in Kazakhstan. It is limited from the north by General Syrt, from the west by the Volga Upland, and from the east by the Pre-Ural Plateau and Ustyurt. The occupied area is about 200 thousand square meters. km and slopes towards the sea.

The northern part of the lowland has heights of up to 100 m, and the southern part lies 28 m below sea level. This flat, drainless plain is composed of rocks of late Quaternary age. There is no permanent hydrographic network within the Caspian Lowland, although it is crossed by such large rivers as:

• Volga,
• Ural,
• Terek,
• Kuma.

In the summer, small rivers dry up or break up into basins that form lake floods, for example, Kamysh-Samarsky lakes, Sarpinsky lakes. Among the salt lakes, Elton and Baskunchak are well known to everyone.

Note 1

The most large river The Russian Plain Volga crosses the Caspian Lowland in the west. The river has the largest delta in Europe and begins north of Astrakhan. Its main branches are 300-600 m wide, branching into numerous channels and eriks, which are small watercourses up to 30 m wide. Flowing into the Caspian Sea, the Volga is divided into 800 mouths.

The climate of the territory is sharply continental, with average January temperatures ranging from -14 degrees in the north to -8 degrees on the coast. July temperatures vary from north to south from +22 to +24 degrees, respectively. Precipitation falls unevenly. In the southeast of the lowlands, precipitation falls no more than 150-200 mm. To the northwest their number increases to 350 mm. More evaporates than falls out. Dry winds often occur.

The vegetation cover of the Caspian lowland is characterized by steppe and semi-desert vegetation. It changes from north to south from the feather-grass-forb steppe, south of the feather-fescue steppe, to the wormwood-grass semi-desert in the south. Meadow vegetation covers large estuaries and is represented by thickets of wheatgrass. Vegetation cover is thinning in desert areas.

The lowland vegetation is used as pasture for livestock. Melon growing, horticulture, and vegetable growing are practiced in the Volga-Akhtuba floodplain.

Table salt is mined from salt lakes. On the territory of the Caspian lowland there is the Ural-Emba oil and gas region and oil and gas production is underway.

Fauna of the Caspian Lowland

Within Russia, on the coast of the Caspian Sea, the Volga-Ural interfluve stands out, where the best pastures are located, hunting and fishing are developed, as well as the Ural-Emba interfluve with known oil and gas reserves.

The deserts of the Caspian lowland are home to 56 species of mammals, 278 species of birds, 18 species of amphibians and reptiles. A number of species fall into the category of rare and endangered. The Caspian coast has great importance for migratory and wintering birds. According to experts, about 1.5 million waterfowl winter within the southern Caspian Sea.

The northern and northeastern Caspian coast is a migration area for about 3 million shorebirds. 2.5 thousand pairs of mute swans nest in the reed thickets, 500 pairs gray geese More than 2 thousand pairs of dabbling ducks gather here to molt in the summer.

In this area, 20 thousand pairs of gulls and terns, and up to 1 thousand pairs of pink pelicans have made their nesting grounds.

Note 2

The main population of commercial ungulate mammals is concentrated in the Volga-Ural interfluve - the saiga, the population of which numbers up to 300 animals. At the beginning of 2009, Nature Management and Protection Service environment noted that in the Akhtuba area, groups of saigas of 10-12 individuals were recorded. In the Volgograd region their number was up to 100 individuals. In the summer of the same year, 1.5 thousand saigas were recorded entering from the territory of Kazakhstan. This indicates their spontaneous movement from one territory to another, which greatly complicates full monitoring and protection.

The Caspian seal appears in the waters of the northern part of the Caspian Sea in winter and spring, the population of which ranges from 450-500 thousand individuals. Five species of animals are numerous:

• fox,
• steppe polecat,
• wolf,
• saiga,
• Eversman's hamster.

More than 30 species are common in the region; the remaining species are found in the Caspian deserts.

Endemics include the long-spined hedgehog - a rare species of insectivore, with a body weight of up to 750 g and leading a nocturnal lifestyle, the Ustyurt mountain sheep of the bovid family of the artiodactyl order, the honey badger - the only species in the mustelidae family, the Caspian seal - an inhabitant of the entire water area of ​​the Caspian Sea, but in the cold time of year concentrated on the northern coast of the Caspian Sea, Bobrinsky's leather jacket - bat order of bats. These animal species are endangered.

Very low level the number and density of animals such as gerbils and jerboas. IN last years it is up to 6 individuals per 1 hectare. The number of gophers is even lower - 3 individuals per 1 hectare. A significant role in the region is played not only by valuable commercial species- saiga, fox, steppe polecat, but also those who are carriers of infectious diseases - jumping jerboa, gray hamster, gerbils.

Environmental problems of the territory

One of environmental problems territory is associated with rising levels of the Caspian Sea. The result of this was the flooding of vast areas of the Caspian lowland, flooding of port facilities, settlements, transport communications, etc. The rapid growth of cities, the saturation of industrial enterprises, the activities of which contribute to the pollution of the Volga and its tributaries, the plowing of land and improper agricultural practices accelerate development erosion processes.

The territory of the Republic of Kalmykia is overloaded with pasture lands, where haphazard grazing of livestock is carried out. The result is desertification and loss of grass. In order to prevent desertification of Kalmyk lands, the “Federal Program to Combat Desertification of the Territory” is in effect. There are first positive results in resolving this issue.

Another pressing problem is the pollution of the Volga water. Flowing through the entire Russian Plain and receiving untreated water from enterprises along its entire length, the river carries it into the Caspian Sea, creating an unfavorable environmental situation in the area. As a result of pollution of the Caspian Sea, its biodiversity is reduced, alien bacteria penetrate, and pollution from land-based sources occurs.

Note 3

The main pollutant is oil, which suppresses the development of phytobenthos and phytoplankton. The sea served as a testing ground for the introduction of new species, but with the penetration of alien organisms from other seas, events began to develop according to a dramatic scenario. An example of drama is the mass reproduction of the ctenophore Mnemiopsis. Appearing for the first time in the Sea of ​​Azov, it literally devastated it, and penetration into the Caspian Sea was not difficult. Feeding on zooplankton, the ctenophore destroys the food base of Caspian fish. Having no natural enemies, and quickly multiplying, it has become out of competition with other consumers of plankton.

Oil pollution negatively affects heat-gas-moisture exchange between the water surface and the air basin. The rate of water evaporation decreases several times.

Oil pollution affects waterfowl, the feathers of which lose their water-repellent and heat-insulating properties. As a result, birds die in large numbers. Oil spills also affect other animals of the Caspian lowland, for example, the number of sea pike perch is declining.

The construction of hydroelectric power stations on rivers also leads to undesirable consequences - fish are deprived of their natural habitats, river beds begin to silt. Fortunately, a protected area has been created in the northern Caspian Sea and an appropriate regime has been introduced, which prohibits any geophysical work.

Note 4

To eliminate or at least somewhat mitigate negative environmental phenomena, large investments are required. But, unfortunately, enterprises do not have available funds for these purposes. The Caspian Sea and its northern shores continue to gradually become polluted