lakes – russiangeography.com https://russiangeography.com Just another WordPress site Sat, 17 Mar 2018 14:55:00 +0000 en-US hourly 1 https://wordpress.org/?v=6.0.1 https://russiangeography.com/wp-content/uploads/2021/12/cropped-icon-32x32.png lakes – russiangeography.com https://russiangeography.com 32 32 Lake Ulahan-Ary-Kuele https://russiangeography.com/central_siberian_plateau/lake-ulahan-ary-kuele https://russiangeography.com/central_siberian_plateau/lake-ulahan-ary-kuele#respond Sat, 17 Mar 2018 14:55:00 +0000 https://russiangeography.com.daggettlake.net/lake-ulahan-ary-kuele/

Lake Ulahan-Ary-Kuele

The unique lake Ulahan-Kuel is one of the most protected natural areas of Yakutia, it has the status of republican significance. It is located in the northeastern part of the Žigansky ulus. The total area is 11046 ha.

It is unique in its origin water body, which has a special nature protection, scientific, cultural, aesthetic, recreational and health value, which is of special economic, social and historical value for present and future generations.

A special regime for the use and protection of a unique lake is established with the aim:

  • – conservation of Lake Ulahan-Kuel in the natural state;
  • – reproduction and restoration, as well as rational and regulated use of aquatic biological resources;
  • – Conducting ecological monitoring and propaganda of nature protection.

Calm water surface and towering on its backdrop are extremely clear silhouettes of mountains with white veins of snow … Ice at the water edge and untouched virgin forests – all this can be seen in a unique place in Yakutia, on a lake, whose name is pronounced correctly the first time, not so it’s easy – Ulahan-Ary-Kuele. There are a lot of beautiful places in Yakutia, but even against their background this amazing lake, considered a special nature protection zone, stands out from the general number.

The beautiful, mysterious, somewhere even mystical Lake Ulahan-Ary-Kuele is located on the island, which in itself is already quite unusual. This island is called as difficult to pronounce, how beautiful is its nature – Ulahan-Ary. In addition, the island is uninhabited, and, hence, problems with crowds of tourists here will not be exact.

Ulahan-Ary is characterized by the fact that there are quite a lot of water reservoirs on its territory and the largest of them is just Ulahan-Ary-Kuele. But his main advantage is not in impressive proportions, but in stunning beauty. The lake was not accidentally included in the list of specially protected natural sites. The flora and fauna of the island and the lake itself are rich. Deer, moose, bears, sables, who just do not live on a densely forested island. The underwater lake world is also rich, and by the way, it allows fishing, that is, it is quite possible to taste the local rare varieties of fish. The water in the lake has an unusual color, especially in combination with local vegetation. And its depths are not great: a maximum of 4 m. But you should not swim here, no matter what.

Address: Anabar National District, Republic of Sakha. To get there by public transport is impossible, it is necessary to negotiate with the driver of the all-wheel drive jeep, which will deliver for 4 hours from Taimylyr. The nearest village is Ust-Olenek, about 50 km from the lake.

]]>
https://russiangeography.com/central_siberian_plateau/lake-ulahan-ary-kuele/feed 0
Lake Manych-Gudilo https://russiangeography.com/nature_reserves/lake-manych-gudilo https://russiangeography.com/nature_reserves/lake-manych-gudilo#respond Thu, 16 Oct 2014 11:18:00 +0000 https://russiangeography.com.daggettlake.net/lake-manych-gudilo/

Lake Manych-Gudilo

The largest lake in the Rostov region is Manych-Gudilo – relic, tectonic, the so-called lake-saucer. The lake of more than 150 km in length, and up to 10-15 km (in some places) in width; its depth – 4 m or more. On the shores of Lake Park is bordered with Kalmykia, Stavropol Territory, the proletarian district of Rostov region. Lake Manych- Gudilo water salinity exceeds almost twice the salinity of the Black Sea, is one of the largest lakes in Europe. Here there are a small, southern, and the three-spined stickleback, pipefish – that’s all, perhaps, that can live in a salt water.

The stark beauty of Lake Manych-Gudilo, contrast and somewhat unpredictable occurring in it natural phenomena, poorly studied many of them gave rise among people living in the vicinity of legends and tales.

Strong winds that prevail in these areas, raise the lake big waves that noise beating on the shore, in some places, their height reaches 12-15 meters or more. Hum their spread far around the area. Howling of the wind over the steep banks in numerous ravines complements this range buzzing sounds, which gave the name of the lake – Gudilo. Hum can be heard in some parts of the lake and in calm weather.

In the center of the lake is the island Vodnyi, where more than 50 years lives a herd of feral horses. Free herd – one of the attractions of the Nature Reserve “Rostov”. No one knows how and when to put the horse on the island Vodnyi. Island 12 km long and up to 4 km sheltered settlers, there is only fresh water. Therefore, watering horses in the summer, when the air temperature reaches 30 – 40 degrees, being the reserve staff. Thanks to the care of the reserve, the number of horses in the herd is now more than 300. A 10 minute walk along the shore of the island opens eyes another small island – “Bird.” Its length 100 m, width up to 20 meters. Here we are already seeing the cane, which indicates the presence of fresh water springs on the island. Breed on the island: spoonbills, gull-Gull, Little Egret, mute swans, sometimes the Dalmatian pelican, etc.

Driven by the memory of hundreds and thousands of generations, countless flocks of birds congregate each year on the waters, islands and shores of lakes Manych. That is why, as the main way of flight and place seasonal aggregations of waterfowl lake Manych-Gudilo included in the list of objects of the international Ramsar Convention on the Conservation of Wetlands and the Island portion of the reserve is recognized as an important bird of international importance.

“Starikovskii” section of the reserve.

“Starikovskii” section of the reserve is located in the east of the Orel district and has an area of ​​2,182.5 hectares.

Feature of its territory is a large number of ravines. On the slopes of the surface outcrops of crystalline gypsum veins. Separate crystalline aggregates grow large and a weight of several kilograms. As in the Geological Museum, can be found here growths of crystals in the form of “rose” and “dovetail”. On the bottoms of the beams whiten yields salt, and many streams are strongly mineralized. Along the saltwater creeks and on the bottoms of the beams developed original vegetation of saline soils. Grow Salicornia, halophytes, salt-tolerant sarsazan and other plants. In the early summer thickets Salicornia have the form of bright green lawns lush vegetation. With the approach of autumn frosts in their tissues formed pigment anthocyanin, which gives red stems. Of burnt autumn steppe lawns and stream beds beams covered glasswort, look very unusual.

Also on this site marked grasses: Lessing, Ukrainian, hair, etc; well presented meadow vegetation involving Sitnik Gerard, reed land, limonium gmelinii and limonium Sarepta, quack grass, sedges and other. On the Old site is Lysianka pond – huge fresh water created by human hands. He appreciated the bird world. Here you can find swans majestically and gradually floating in the clear waters, coot, common shelducks, geese, grebes and many other birds.

In a large number of near ponds accumulate Demoiselle cranes. On some days here were recorded accumulations of up to three thousand of these birds at the same time. A little in Russia such places where you can meet in such a large number of Demoiselle cranes, which is why this bird has become a symbol of the reserve. About pond vegetation includes reed, bulrush, cattail, sedge. Interesting and original form are plants tumbleweeds.

“Krasnopartizanskiy” section of the reserve.

“Krasnopartizanskiy” site is located 5 km south-east of the “Starikovsky” plot Remontnensky area and covers 1768 hectares. On the boundaries of this area are growing forest plantations, where they found their permanent place of residence of rooks, falcon, kestrel. Steppes of this part of the reserve known as a place of clusters on autumn migration flocks Strepetov.

Krasnopartizanskaya Land Reserve – is a typical fescue-feather grass steppe, the dominant vegetation is represented by long-term drought-and frost-resistant plants with strong root system. This feather grass, fescue, sage, wheatgrass, yarrow and other herbs.

Part “Tsagaan-Hag”.

Part “Tsagaan-Hag” is located in the south Remontnensky district. Its area is 990 hectares. This mysterious name of the site is translated from the Kalmyk means “white silt”: lake located on saline site periodically dries up, then on the surface appears white salt, which gave its name to reserved lake.

The site is located in two regions of the Federation: the western part – Proletarian Reservoir – in the Rostov region, the eastern – Lake Manych Gudilo – in the Republic of Kalmykia, within a branch of the state ornithological reserve “black earth.” The western boundary of land is located 160 km south-east from the city of Rostov-on-Don, East – 80 km to the west-south-west from Elista.

Proletarian reservoir is a large reservoir with a maze of lagoons and shallow bays on the North coast. Typical zones reed developed only in freshened areas in gullies and Novo-Manych dam. Breeding, moulting, feeding during migration of wild geese, sandpipers, ibises and pelecaniformes. The area of concentration of migratory geese, ducks and waders.

On the lake. Manych Gudilo due to high salinity, emergent vegetation is almost not developed, and the numerous islands of the reservoir covered with grass-forb associations.

Very high productivity of plankton and benthos. Place for mass nesting colonial waterbirds: gulls, pelicans, wading. District of mass flight and stop during migration of waterfowl, one of the largest in Eurasia clusters migrating geese (white-fronted goose, red-breasted goose, piskulka, gray goose).

]]>
https://russiangeography.com/nature_reserves/lake-manych-gudilo/feed 0
Rybinsk reservoir https://russiangeography.com/lakes/rybinsk-reservoir https://russiangeography.com/lakes/rybinsk-reservoir#respond Mon, 13 Oct 2014 07:35:00 +0000 https://russiangeography.com.daggettlake.net/rybinsk-reservoir/

Rybinsk reservoir

Size: 4580 km2
Maximum depth: 30 m

Rybinsk reservoir is a large reservoir on the Volga river and its tributaries Sheksna and Mologa. Located mainly in the Yaroslavl region, in the North-West, partly also in Tver and Vologda regions. Formed in the late 30’s-early 40-ies of XX century wodoodporne structures Rybinsk hydroelectric station, located in the Northern part of the Rybinsk, overlying beds of two rivers: the Volga and Sheksna. The hydrosystem includes building Rybinsk hydroelectric power 346 MW (original 330 MW), built on the old bed of the Sheksna, ground run-of-river dams and interfacing their dam, a concrete spillway dam and double-strand gateway, built on the Volga course. The value of reservoir: navigation, fishing, power generation Rybinsk hydroelectric station. About 17 thousand years ago on the site of the Rybinsk reservoir was glacial lake. Gradually it became shallow, and there was extensive Small-Sheksna lowland.

Main features.

The shore of the Rybinsk reservoir predominantly low, its coastline stretching wet meadows, forests, swamps. The only places in the valleys flooded rivers can be found cliffs covered with pine trees. The height of the waves up to two meters. With the advent of the Rybinsk reservoir, the climate in the surrounding areas have changed. The summer was cooler and more humid, ceased to grow wheat and flax. In winter, the reservoir is frozen. The ice lasts from mid-November to early may. The average ice thickness reaches 60-70 centimeters. From the North-Western shore of the Rybinsk reservoir often large detached layers of peat, covered with vegetation, and even small trees. They are Autonomous swim across the waters, creating minibosses. The ship channel is away from the coast. Navigation takes an average of 190 days. Ports: Cherepovets – when it falls into the reservoir of the river Sheksna, vesegonsk – at the confluence of the river Mologa. Through the Sheksna reservoir is connected with the Volga-Baltic water system.

Rybinsk sea – giant laboratory of the Institute of biology of inland waters Russian Academy of Sciences. In the North-West of Darwin reserve, specializing in research on the impact of the reservoir on the natural complexes of the southern taiga. Fish stocks of the Rybinsk reservoir are: sturgeon (sturgeon family), whitebait (family clupeidae), vendace and Peled (family whitefish), smelt (family korolkowii), pike (pike family), acne (acne family), catfish (catfish family), burbot (cod family), calf-Golovach (family goby), sculpin (family rogatcheva), eel, loach, loach ordinary (family true loaches). The most diverse family of carp fish: blue bream, bream, white-eye, bystrany, bleak, Chub, bream, crucian gold, silver carp, sneep, carp, gudgeon, Chub, IDE, Dace, a fish, roach, tench, minnow lake and ordinary. The main species of fish caught in the reservoir: bream, roach, Zope, smelt, burbot, pike, walleye, perch. Rybinsk, vodohranilishe accommodates 24,8 billion cubic meters of water.

]]>
https://russiangeography.com/lakes/rybinsk-reservoir/feed 0
Zeya reservoir https://russiangeography.com/lakes/zeya-reservoir https://russiangeography.com/lakes/zeya-reservoir#respond Mon, 13 Oct 2014 07:28:00 +0000 https://russiangeography.com.daggettlake.net/zeya-reservoir/

Zeya reservoir

Area: 2,420 km2
The greatest depth of 34 meters.

Zeya reservoir – dam on the Zeya River in the Amur region of Russia. Zeya hydroelectric station dam formed in 1974-1980, respectively. Reservoir extends upstream from the Zeya hydroelectric dam in Zeya, over a length of 40 kilometers within Tukuringra ridge is a narrow body of water with the bay, which formed at the confluence of the tributaries of the Zeya and upstream within Verhnezeis basin, becomes a body of water. Baikal-Amur Mainline runs along the north coast of the water reservoir and crosses the bay in 1100 meter bridge near the village of Bomnak. Reservoir is used for navigation and fishing (whitefish, trout, pike, Amur catfish, sturgeon and grayling).

Main features.

The area of the Zeya reservoir – 2419 sq. km, complete, and usable capacity of reservoir – 68,42 and 38,26 cubm When creating Zeya reservoir was flooded 3.9 thousand hectares of farmland. In the area flooded by the reservoir, was 14 settlements, inhabited by 4 460 people who were resettled in the newly built and moved towns. Zeya reservoir, volume of water takes 3rd place in Russia, after the common (169,3 km3) and Krasnoyarsk (73,3 km3) of water. Is the source for water supply of the greater part of the city. Reservoir formed recently (about 35 years ago) and biological decay of the upper organic layer of the earth is still ongoing, as evidenced by the dark brown color of the water. This process has stabilized, but noticeable water purification can be expected only in 20-30 years. Water in its composition with low mineral content and high content of biogenic and organic substances.

Environmental problems.

Before the flooding of the reservoir is not fully implemented lesoochistka. The remaining forest slowly decomposes to form phenols. Hydroelectric dam built without rybopodёmnikov, resulting in a natural way barred the passage of fish on the spawning grounds. In addition, the negative impact on fish produce significant, up to 8 meters, the fluctuations of the reservoir level. Lack of shared sudopodёmnikov navigation on two non-communicating portion on the bottom and the upper reach. Zeya River below the dam does not freeze over 80-100 km. Therefore, in the winter time in this interval river transport links broken the ice between settlements. In winter along the ice-free portion of the river is worth a dense fog that has an impact on the health of people in the area. Due to late frost reservoir (December), autumn can be warm, long, cold softened.

]]>
https://russiangeography.com/lakes/zeya-reservoir/feed 0
Bratsk reservoir https://russiangeography.com/lakes/bratsk-reservoir https://russiangeography.com/lakes/bratsk-reservoir#respond Fri, 11 Jul 2014 12:14:00 +0000 https://russiangeography.com.daggettlake.net/bratsk-reservoir/

Bratsk reservoir

Area: 5 426 – 5 470 km2
Maximum depth: 150 m

Bratsk reservoir – a reservoir in the Irkutsk region of Russia, founded on the river Angara in the result of construction of the Bratsk hydroelectric power station, the second on volume of the reservoir in the world. On the banks of the city of Bratsk, by which it was named, and Svirsk. Water is widely used for navigation, fishing, rafting and water supply. A lot of fish resources.

Bratsk reservoir on the river Angara is the biggest on the total volume (169,3 km3) the valley reservoir in the world. The reservoir is filled in 1961-67 years and has a very complex configuration. Consists of two main pools, occupying the flooded areas of the valleys of the rivers Angara (length 500 km, the maximum width 33 km) and Oka (the length of 370 km). In the valleys of many other tributaries formed a long meandering creeks.

Bratsk reservoir is of great importance for energy, navigation, rafting, water and fisheries.

Main characteristics.

The dam of the Bratsk hydroelectric power station was built in 1961, the filling of the reservoir ended in 1967. The surface of the water reservoir ranges from 5 426 km2 to 5 470 km2, and the volume is 169 km3. Useful volume of the Bratsk reservoir is 35.41 km3, mean depth 31 meters, level change during the drawdown on the NPA – 7.08 m, Coastline length of about 7 400 km strongly indented, in the confluence of major rivers – Angara, Oka, and others formed a long bays. The width of the Bratsk reservoir exceeds 20 km.

]]>
https://russiangeography.com/lakes/bratsk-reservoir/feed 0
Onega lake https://russiangeography.com/lakes/onega-lake https://russiangeography.com/lakes/onega-lake#respond Thu, 26 Jun 2014 15:24:00 +0000 https://russiangeography.com.daggettlake.net/onega-lake/

Onega lake

Area: 9700 km2
Maximum depth: 127 m

Onega lake is a lake in the North-West of the European part of the Russian Federation located on the territory of Karelia, the Leningrad and Vologda regions. The second largest lake in Europe after Ladoga. Belongs to the basin of the Baltic sea Atlantic ocean. The lake area without the Islands is 9690 km2, and the Islands – 9720 km2; the volume of water – 285 km3; length from North to South – 245 km, the maximum width is to 91.6 km. Average depth is 30 m, and the maximum is 127 m On the shores of lake Onega are the cities of Petrozavodsk, Kondopoga and Medvezhegorsk. Lake Onega get about 50 rivers, but only one flows out – Svir.

Shore, bottom topography and hydrography of the lake.

The surface area of lake Onega is 9,7 thousand km2 (excluding Islands), length – 245 km, width – about 90 km North shore is rocky, highly rugged, South – mostly low, undifferentiated. In the Northern part of deep into the mainland numerous lips, elongated like ticks cancer. Here is juts out into the lake huge Zaonezhye Peninsula, South of which lies the island of Great klimenetsky. To the West of them, is the most deep (up to 100 m and more) part of the lake – Big Onego lips Kondopoga (with depths of up to 78 m), ilem-Gorsky (42 m), Lizhemsky (82 m) and Unitsa (44 m). South-West from the Big Onego extends Petrozavodsk Onego with its bays Petrozavodsk lip and small Algumas and Bingoboy. To the East of Zaonezhye stretched North Bay, Northern part of which is called Povenets and South Zaonezhie Bay. Deep sections are alternated with banks and groups of Islands, which dismembered the Bay into several parts. The southernmost of these areas – Small Onego depth of 40-50 meters of Many stones on the shores of the lake.

The average depth of the lake is 31 m, the maximum depth in the most deep-sea Northern part of the lake reaches 127 M. the Average depth in the Central part is 50-60 m, closer to the South the bottom rises up to 20-30 meters To lake Onega characterized by numerous pronounced increase and reduction of the bottom. In the Northern part of the lake a lot of gutters, alternating with high rises bottom, forming banks, which often catch fish industrial trawlers. A significant part of the bottom is covered with silt. Typical forms are Ludi (shallow rocky shoals), Selge (deep improve the bottom with rocky and sandy soils in the southern part of the lake), underwater ridges and ridges and trenches and pits. Such relief, creates favourable conditions for fish life. For the regime of lake Onega is characterized by spring water rise, which lasts 1.5-2 months, with annual amplitude of water level up to 0.9-1 m The lake discharges regulated Verhnesvirsky HPP. Rivers bring to 74 % of the income part of the water balance (15,6 km3 per year), 25 % falls on precipitation. 84 % of the expenditure part of the water balance falls on runoff from the lake on the river Svir (average 17,6 km3 per year), 16 % – on the evaporation from the water surface. The highest water levels of the lake in June – August, the lowest – in March – April. There are frequent unrest, storm waves reaching up to 2.5 m high. The lake freezes in the Central part in the middle of January, in the coastal part and bays, in the end of November – December. In late April, opened the mouth of the tributaries, the open part of the lake in may. Water in open deep parts of the lake is transparent, with visibility up to 7-8 m In bays a little less, up to one meter or less. Fresh water with salinity of 10 mg/L.

Flora and fauna.

Low coast of Onego lake wetlands and flooded when the water level rises. On the banks of the lake and its Islands, in the reed and the reed-beds, there are ducks, geese and swans. The coastal area is covered by dense taiga forests in pristine condition. Lake Onega is distinguished by great variety of fish and aquatic invertebrates, including a significant number of relicts of the ice age. In the lake there are sterlet, salmon lake, lake trout, trout, char Luna, Paliy pit, whitefish, vendace-kylec, whitefish, grayling, smelt, pike, roach, Dace, silver bream, bream, sabrefish, Golden carp, trout, loach, catfish, eel, pike, perch, ruff, slingshot Onega, bullhead, burbot, lamprey eel river and brook. Just Onega lake meets 47 species of fish belonging to 13 families and 34 species.

Islands.

The total number of Islands in the Onega lake reaches 1650, and their area is 224 km2. One of the most famous Islands in the lake is the Kizhi island is situated on the homonymous Museum-reserve with built in XVIII century, the wooden churches of the Transfiguration and intercession. The largest island is a Large klimenetsky (147 km2). It is located several towns and a school. Other Islands: Big Lelikovsky, Suyari.

]]>
https://russiangeography.com/lakes/onega-lake/feed 0
Chany lake https://russiangeography.com/lakes/chany-lake https://russiangeography.com/lakes/chany-lake#respond Thu, 26 Jun 2014 06:28:00 +0000 https://russiangeography.com.daggettlake.net/chany-lake/

Chany lake

Area: 1400-2000 km2
Maximum depth: 7 m.

The Chany lake – closed salt lake in Russia, located in Barabinsk lowland on the territory of the Novosibirsk region, the largest lake in Western Siberia. The lake is located on the territory of five districts of the Novosibirsk region: Sivinskogo, Barabinsk, Janovskeho, Kopynskoho and Chistoozernoe. It got its name from the word Chan (Turkic) is the vessel of the big sizes. The Chany lake is located at the altitude is 106 meters above sea level. The lake has 91 km, 88 kilometers in width. The lake area is variable and currently, according to different estimations makes from 1400 to 2000 km2. Average depth of about 2 metres. The basin of the lake is flat. The lake is shallow with depths of up to 2 meters account for 60 % of the total lake area. The lake shore is low and highly rugged, overgrown with reeds, the reeds, sedge and bushes. The bottom is sandy and muddy. The maximum recorded temperature of water in summer is 28,3 C. a Large part of the lake located in the forest-steppe natural zone.

On a lake about 70 Islands, the largest are Amelkina Mane, Shundikov, Lean, Bear, Cap, Chinaaa, bird-cherry, Rare. Island Cheremushkin, Mare, Perekupnoy, Bekarev, guelder rose, Chinaaa, Sipiagin, Round, Kolotov, Kamyshnyi are natural monuments in the region, because they contain unique landscape, which is the habitat of rare species of plants and animals. Among the largest peninsulas – Zelenchuk, Kondakov, Naked, waskin, Cape, Travnikov, Rodyushkin, Kvashnina, Malinina, Dark, Tyumen. The Islands and the Peninsula of the lake have a characteristic feature of most of them stretched from South-West to North-East. Their specific location due to the fact that they represent a half-mane. The salted lake, in the South-Eastern part of the lake salinity below. The power of the lake mainly snow, lake fed by rivers Kargat and the Chulym river (flows into Small Tanks). Earlier in the lake flowed the river Sarika, connecting it with lake Sartlan. Average annual total flow of the river Chulym and Kargat not very significant and is 0,44 km3, while drains are very IZMENChIVOSTI Vats is a unique reservoir of Western Siberia. The maximum value of the total flow was achieved in 1948 – 1,72 km3, the minimum – in 1968, when it was 0,013 km3. The inflow of water has a tendency to decrease due to the many dams built on recasa connected with channels with more fresh Small lakes Chany and Arcul. The lake is a system of pools connected by canals and shallow water zones, of which the largest three: Kireichenko, Tagana-Kazantsevo and Yarkovsky different mineralization of water, space, water, soils, prey base . Freezes in the second half of October to the first half of November, opened in may. On the lake there is a local shipping.

Climate.

The climate in the area of lake Chany continental. The average January temperature is -19,7 degrees C, in July – +18,3 C. frost-free period lasts from 115 to 120 days. The average annual rainfall is 380 mm snow cover thickness – 20-30 see

Flora and fauna.

The Chany lake is inhabited by 16 species of fish. The most numerous: silver carp, perch, carp, IDE, pike-perch. The average number have roach, pike, bream. Small species – Golden carp, Peled, eel, tench, lake minnow, gudgeon, verkhovka. Main place of wintering of fish – Jarkovsky ples and lake Arcul. The most numerous fish in Harkovskom ples – perch. In summer Kireichenko ples in a significant number inhabited by all basic kinds of fish fauna in Tagana-Kazantsevo the reach of the common species are IDE, pike, carp, crucian, a smaller number of roach and perch. In dry years the winter Zamora cause enormous damage in fish populations, especially valuable commercial species. In dry periods killed a large number of eggs and young, so the fish tank is required. The lake regularly serebryatsya, it holds the commercial cultivation of fish. First fish-breeding work in the lake began in 1926 – 1927. Originally were acclimatized carp, carp, bream. Later was conducted acclimatization Sudak, Peled, tench, nelma, muksun, Baikal omul, when the stocking of the lake accidentally universe verkhovka. The first attempts of acclimatization great success is not achieved, increasing catches were observed. Further acclimatization perch was successful, and he reached great numbers. The bulk of bream dies in dry years when Zamora, so its population has not yet reached the commercial level. At present reliable information about the presence of the lake Baikal omul and nelma not. The failure of the omul is explained by the fact that the lake for this type of fish is shallow. Acclimatization Peled failed because of the high salinity of the water, and at the present time commercial cultivation of Peled, when the larvae grown in fish farms, are released into the lake, and fish grow to commercial size. In addition, many larvae omul, muksun, Peled and nelma was eaten perch, roach and IDE.

In 1976 on the river Chulym was built fish hatchery “Urumqi”, including those engaged in growing and stocking of the lake Chany the young of carp. Active stocking juveniles weighing 25 – 80 grams led to the fact that the lake has been formed by numerous self-reproducing population of carp. According to the observations of the Novosibirsk branch of “Sibribniiproekt” in 1993 carp on the number of juveniles appearing ahead of native species of fish, roach, IDE and perch. The economic crisis of the 1990-s led to the fact that the scale stocking lakes kennel has significantly decreased.

Fish stocks are now in comparison with the nineteenth century much drooped. For the first time reduction in the catch of pike, carp and perch was registered at the end of the XIX century: “… the first was full of fish, in it there were pikes to pood weight, carp and perch from 5 to 7 – 8 F. Now, for unknown reasons, fish his wealth emaciation and the fish were crushed”. In XX century in periods of high water levels in fish catches reached 10 thousand tons per year in dry years was reduced up to 200 tons per year. In dry periods the basis of commercial catches occupy low-value fish species. Among the main reasons for the reduction of catches are named the following: the Decline and sharp fluctuations in water level. Winter kills. Freezing to the bottom of a significant part (up to 25 %) of the lake in winter. Reducing stocking. Anthropogenic impact. In the lake officially permitted fishing nets at the purchase of the corresponding license. The established quota on catching the fish is 2800 tons per year. Ichthyologists believe the actual catches are much higher than the official statistics, in addition, in recent years on a large scale is poaching. Increasing concentrations of phenols, oil products, nitrogen compounds and other substances. High mineralization of water in the lake. The most saline water noted in Kireichenko (6 g/dm3) and Harkovskom (2.5 g/dm3) reaches. At the end of XX century the lake has got the form of the goldfish called Amur carp. Amur carp for several years a rapidly multiplied, virtually ousted from the lake did not bear with it competition Golden carp, and currently ranks first in catches. Part of the population perch infected Gill tick. Opisthorchiasis in fish lake Chany reported so far.

The lake plays an important role in the migration of many species of water birds: ducks, gulls, geese, waders, swans, terns, coots, mountain duck. Out of the rare species of birds on lake marked white-headed duck, red-breasted goose, Asian Dowitcher, sociable lapwing, Avocet, black-winged stilt, great black-headed gull, Caspian tern, steppe circosta, Golden eagle, white-tailed eagles, Dalmatian Pelican. On the lake there are significant aggregations of waterfowl in periods of migration and molting. During migration and nesting on the lake is up to 220 species of birds, according to other data – up to 300 species of birds. In the 1970-ies estimates ornithologists on the lake for the season used to 1.5 million waterfowl. During the XX century has been a steady decline in the number of waterfowl because of mass destruction. For example, in 1930 in the system Chanovsky lakes were collected 9 million eggs and many more damaged. At the beginning of the XXI century the main anthropogenic factors that reduce the number of birds were the destruction of nests during grazing in the coastal part of the lake, bird mortality in fishing nets.

From mammals inhabit the lake muskrat, in the forest-steppe lands, timed to the lake, inhabited by foxes, hares, ROE deer, badgers, foxes, weasels. The lake is rich in plankton, as zooplankton and phytoplankton. According to the data of 1983 are found in the lake 404 species of algae. In Kireichenko ples noted the high biomass of algae, strong development of phytoplankton has a negative impact on the abundance of fish. Species diversity of zoobenthos small, dominated by midges, also there are shellfish, caddisflies, KOLIZEY, gammarids, oligochaetes, dragonflies, mayflies. On the banks and Islands of the lake grow birch, cherry, cranberry, aspen, hawthorn, dogrose, currant, raspberry, fern. In 1940-ies on the Northern shore of the lake were planted with oak and pine forest. On some Islands, for example, on the island Skorecki grow and flower wild peonies.

]]>
https://russiangeography.com/lakes/chany-lake/feed 0
Lake Khanka https://russiangeography.com/lakes/lake-khanka https://russiangeography.com/lakes/lake-khanka#respond Thu, 26 Jun 2014 06:18:00 +0000 https://russiangeography.com.daggettlake.net/lake-khanka/

Lake Khanka

Area: 4070 km2
Maximum depth: 11 m

Lake Khanka is located on the border of the Primorsky region of Russia and the Heilongjiang province of China. Khanka is the largest freshwater reservoir in the far East. The area 4070 km2 (with an average water level), length 95 km, dominated by the depth of 1-3 m, maximum – 10,6 m flow Into the lake, on 16 rivers, particularly Muddy, Melgunovka, the komissarovka river; flows the river Sungacha, a tributary of Ussuri river (Amur river basin). The Khanka lake and the adjacent territory are unique on biological diversity. Here are common meadow plant communities, grassy bogs, oak forests and woodlands, with the participation of pine grave. The lake is home to a large number of freshwater fish and other aquatic organisms. The presence of large freshwater reservoir led to the concentration of huge numbers of waterbirds. Of protected areas there is Khankaisky nature reserve.

General description.

The Khanka lake is the largest lake of Primorsky Krai is located in the centre Khanka lowland on the border with China Heilongjiang province.
The Northern part of the lake belongs to China. The lake – pear extension in its Northern part. Surface water is variable, it changes depending on climatic conditions. The maximum reaches 5010 km2, minimum – 3940 km2. The length of the lake is about 90 km, the maximum width is 67 km In the Khanka lake flows into 24 river, only one flows out – Sungach, which connects it with the Ussuri river, and the latter in turn with the Amur river. The Khanka lake is a shallow lake with an average depth is 4.5 m, and prevailing depths of 1-3 m, maximum depth is 10,6 M. Water in the lake is muddy, because of the frequent winds, and consequently strong mixing. The average runoff in the lake equal 1,94 km3 per year from a lake near – of 1.85 km3. Freezes in the second half of November, opened in April. Varied fauna and flora of lake Khanka. In 1971, in accordance with the Ramsar Convention, this territory was assigned the status of wetlands of international importance. And in 1990 in the basin of lake Khanka is organized by the state nature reserve Khankaisky. In April 1996 between the Governments of Russian Federation and people’s Republic of China signed the agreement on creation on the basis of Khankaisky nature reserve in Russia and Chinese reserve “Xingkai-Hu” of international Russian-Chinese nature reserve “Lake Khanka”.

The wetlands in the basin of lake Khanka are a unique natural complex. Khanka lowland and the coast of the lake are quite wetlands. Characteristic of Khanka so-called Plavni – plant communities formed by different kinds of sedge and grass. They form strong turf, covering the water table on the many tens of square kilometers. Here presents meadows (from wetlands to steppe, meadow-forest, forest-steppe and steppe plant communities. In the lake is home to many species of fish and aquatic invertebrates, many of which are endemic. The lake lives 52 species of fish, such as carp, verkhoglyad, carp, catfish, snakehead. On the banks of the nest and stop during migration birds of all kinds.

]]>
https://russiangeography.com/lakes/lake-khanka/feed 0
Lake Taimyr https://russiangeography.com/lakes/lake-taimyr https://russiangeography.com/lakes/lake-taimyr#respond Wed, 25 Jun 2014 12:55:00 +0000 https://russiangeography.com.daggettlake.net/lake-taimyr/

Lake Taimyr

Area: 4 560 km2
Maximum depth: 26 m

Lake Taimyr on the Taimyr Peninsula in the Krasnoyarsk Krai of the Russian Federation, is part of Taimyr nature reserve. The second largest after lake Baikal in the Asian part of Russia. Taimyr is the most Northern in the world this large lake is its extreme Northern point is North of 75 degrees North latitude. From oz. Taimyr follows R. bottom of Taimyr. The lake is covered with ice from late September to July, the average duration of the ice-free period – 73 days. The water temperature in August is +8 degrees C, in winter – slightly above zero. Permanent settlements there, on the lake is located inactive meteorological station.

General description.

Is far beyond the polar circle, in the foothills Byrranga. Coastline is highly indented shallow bays and coves. Gentle southern coast is friable deposits of Quaternary period. North shore, with outputs of older rocks, rises sharply to the foothills of Byrranga, which in Taimyr into numerous tributaries. Some of the rivers start from mountain lakes, such as lake Levinson-Lessing. In the Western part a lot of rocky Islands, in the Eastern part is a sandy island Sokolova-Mikitov. The lake district is located in the climatic zone of tundra, widespread distribution of permafrost. The average annual temperature in the area is -13,4 °C, the average temperature of the warmest month – July – +12,3 C. Despite the large amount of precipitation in winter, the formation of large snow cover hampered by strong winds and flat terrain. In the summer of frequent storm, during which there is a strong turbidity of the water due to the shallow depth of the lake. For the characteristic lake level rise from early summer until August, followed by its decrease until the following spring, during which lost up to 75 % of water. Level change during the year leads to a significant – up to 30-50 % of the area of the mirror, to 84 % of the total lake Taimyr freeze to the bottom during each winter, including up to 25 % of the permanent lake waters. Seasonal decline in the water level can reach a height of 1.5 m above sea level and the area of lake Taimyr – shrink to 1 200 km2. The shallow depth and the water level dropped on average by 5.9 m in winter leads to deformation of the ice cover and propagation. The thickness of ice reaches 2-3 m, crack formation with the subsequent fall of ice accompanied by severe crackling noise.

Flora and fauna.

Despite its location in the lake is 20 species of fish. The most common species such as whitefish, whitefish, whitefish. Also found pike, omul, whitefish, grayling. In small amounts present Siberian sculpin. The Peninsula is inhabited by the following representatives birds: ducks, geese, swans, rough-legged Buzzards, swans, peregrine Falcon. Wintering birds fly away to warm countries, in the summer of return, in order to produce offspring. An interesting phenomenon observed in the lake Taimyr is the lack of higher aquatic vegetation, at a time when there are individuals related to marine aquatic complex and Baikal. In the Taimyr Peninsula is populated Arctic fish whitefish, whitefish, trout and others In the lake there are no representatives of the higher aquatic flora aquatic food chain of animals is based on the phytoplankton. During the winter the water falls amount of dissolved oxygen, since in summer the place demolished many organic substances. Perignane precipitation makes the area very deep depression unavailable for fish. Fauna of lake Taimyr were studied on the subject of adaptation dwelling in him types and possibilities of their resettlement in the Siberian reservoir, which also differ in significant changes during the year. Mainly in the Taimyr flora and fauna aquatic complex living organisms, there are also species characteristic of the lake Baikal. The appearance of the first species explain the message of the lake with the sea through the Lower Taimyra and changes of level of the world ocean in different historical periods. The presence of representatives of the Baikal ecosystem due to glacial periods, during which the hydrological regime of the region fluctuated with the formation of large glacial lakes in North Asia. The island of Taimyr are nesting grounds for migratory birds – the red-breasted goose, geese and other

Climate.

Lake Taimyr located in the severe North conditions of tundra and forest tundra. Here almost everywhere there is permafrost. In the area of lake Taimyr climate is slightly warmer than the other territory of the Peninsula. The average temperature throughout the year does not exceed -13,4 C in the warmest month July is +12,3 C. in Winter the region is characterized by persistent precipitation. While strong wind and plains prevent the formation of large snow layer. In summer, on the Peninsula of the sun is shining all day, shining with rays of the water surface of the lake. During this period, the lake becomes alive. In summer the lake is characterized by storm. Polar summer and Arctic winter to adjust their operations flora and fauna of the area. The plants grow faster, accelerating periodicaled. Chicks faster than in other climatic zones. All life is trying to pass through stages of development, during the short polar summer time. In the tundra, no germs, so warm-blooded organisms are easier to tolerate low temperatures. Ultraviolet rays, which are here in abundance, enhance the overall tone of organisms and at the same time, clean the air from germs. It is believed that in the summer in the tundra people will feel much better than usual climatic conditions.

]]>
https://russiangeography.com/lakes/lake-taimyr/feed 0
Lake Pyasino https://russiangeography.com/lakes/lake-pyasino https://russiangeography.com/lakes/lake-pyasino#respond Wed, 25 Jun 2014 12:02:00 +0000 https://russiangeography.com.daggettlake.net/lake-pyasino/

Lake Pyasino

Area: 735 km2
Maximum depth: 10 meters

Lake Pyasino – lake of glacial origin in Russia, in the South-West North-Siberian lowland in the Krasnoyarsk territory, approximately 20 km from Norilsk. Freezes at the beginning of October, opened from ice in late June – early July.

Physical features.

Flows from the lake only the Pyasina river, the main tributary, R. Norilsk, the latter can be considered upstream of the Pyasina river, which is in the North of modern lake podprugin range end moraines. Norilsk at the confluence of the lake forms a river Delta, part of which is also a river Barn. Other tributaries of the lake are not significant.

Bank of Pacino mostly flat, swampy places. The lake gathers the waters of large lakes Lama, Chum salmon and Deep in the mountains of the reserve. The lake is rich with fish, it meets brown trout 2 types and special types of Chir, called maccuhal.

Pasino is a lake, which is of glacier origin. It is situated in the southwestern part of the lowlands of the North-Siberian on the territory of Krasnoyarsk territory, approximately 20 kilometers from Norilsk in Russia.

Freezes the water reservoir at the beginning of October, and opened the ice at the end of June or in early July. From Pacino one follows the Pyasina river. Main tributary is the river of Norilsk, which is considered the upper reaches of the Pyasina river. This river in the Northern part of modern lake significantly podprugin moraine ridge end. The river at the confluence of the Norilsk in this lake forms the Delta of the river, part of which is the river Barn. Other tributaries of lake Pyasino are insignificant.

Bank of Pacino largely flat, in some places, swampy. The lake includes the waters of large rivers such as Salmon, Lama and Deep.

As already noted, Pyasino lake is located in the Northern part of Eastern Siberia. This pond occupies the bottom of the ancient glacial valley, which is partitioned in the Northern part of the shaft of moraines. The length of Pasino is 70 kilometers with a maximum width of 15 km. The total water area of 735 square kilometers with a catchment area of 24,000 square kilometers.

As noted, in this lake into numerous small rivers. The main tributaries of the pond is a small river Nerilka, pike, Samoyed and a Barn. Pacino are considered to be small reservoirs.

Basically the shores of lake flat, in some places they are swamped, but at the same time, with uenoi, and the Eastern side of the pond is surrounded by small hills covered with forests.

The power of Pacino rain and snow. Annual changes in the level of the surface can reach six and a half meters. In the lake Pyasino is full of fish. However, as already noted, in 20 kilometers from lake is located the town of Norilsk, which has a negative impact on the ecological purity of the water body.

Lake Pyasino is very attractive. It attracts a huge number of fishermen excellent facilities and delicious fish. however, however, to reach the lake is not so easy. This is the mystery of this reservoir. In the summer, access to the lake it is quite problematic to any transport. In winter time all the way hides a solid layer of snow. And what can you do? Any vehicle, getting to a huge lake Pyasino, will struggle to overcome the swampy approaches and are not always able to cross numerous unpredictable, in some places even dangerous, rivers and streams. Crossing of them are known only to a few.

If to speak about crossing the lake, it can be compared with exciting and unpredictable adventure. Lucky – unknown. The wire on this reservoir compared with many kind of lottery, where the rate may be a whole life. Smooth surface of the lake Pyasino very deceptive. In a matter of seconds water can turn into a nightmare for inexperienced sudogoda. Storms on Pacino has long been considered the parables of the town and killed a large number of ships and people. Among other things, the waterway to the lake is only possible for only several weeks. However, however, the scenery of lake Pyasino attract and are attracted by its beauty and unpredictability. Many nature of this area attracts everyone. For this reason many people want to see and to enjoy a truly wonderful and unique species, which cannot be seen anywhere. And for the fishermen, this lake is the gold, for the reason that there are a variety of fish species and abundant.

]]>
https://russiangeography.com/lakes/lake-pyasino/feed 0