Yaik

The Ural, also known as the Yaik , is a river flowing through Russia and Kazakhstan in the continental border between Europe and Asia. It originates in the southern Ural Mountains and discharges into the Caspian Sea. At , it is the third-longest river in Europe after the Volga and the Danube, and the 18th-longest river in Asia. The Ural is conventionally considered part of the boundary between the continents of Europe and Asia.

The Ural rises near Mount Kruglaya in the Ural Mountains, flows south parallel and west of the north-flowing Tobol, through Magnitogorsk, and around the southern end of the Urals, through Orsk where it turns west for about , to Orenburg, where the river Sakmara joins. From Orenburg it continues west, passing into Kazakhstan, then turning south again at Oral, and meandering through a broad flat plain until it reaches the Caspian a few kilometers below Atyrau, where it forms a fine 'digitate' (tree-like) delta.Ural River Delta, Kazakhstan
(NASA Earth Observatory)

Etymology

The river was called (Daïkos) by Ptolemy in the 2nd century AD. Yulian Kulakovsky reads this as Turkic " Jajyk" or "Яик" and on this basis identifies the Huns as Turkic speakers. However, Gerard Clauson disputes that the name could be of Turkic origin as early as the 2nd century, and instead attributes it to Sarmatian origin. Also, the version of origin from the ancient Finno-Ugric and subsequent adaptation by other language groups has not been sufficiently studied (the river originates in the alleged ancestral home of the Finno-Ugric languages). In modern Finno-Ugric, the closest surviving forms are found: "joki" (Finnish), "jogi" (Karelian), "jā" (Mansi), "ju" (Komi) – river, "jəŋk" (Khanty) – water. Also, hypothetically Finno-Ugric titles may have tributaries of the Yaik River, for example Ilek (Erzya "Ilyk" – strength) and Utva (Komi "Ytva" – spring water). In the 10th-Century work ''De Administrando Imperio'', Byzantine Emperor Constantine VII Porphyrogenitus referred to the Ural River as the "Geich." The name Яйыҡ (Yayıq) is currently used in the Bashkir language and Жайық (Zhayıq) in Kazakhstan. In later European texts it is sometimes mentioned as ''Rhymnus fluvius'' and in the Russian chronicle of 1140 as Yaik. The river was renamed Ural in the Russian language in 1775, by Catherine II of Russia.

History

In the 10th to 16th centuries, the city of Saray-Jük (or Saraichik, meaning "small Sarai") on the Ural River (now in Atyrau Province of Kazakhstan) was an important trade center on the Silk Road. In the 13th century, it became a stronghold of the Golden Horde. It was destroyed in 1395 by the army of Timur but then rebuilt to become the capital of Nogai Horde in the 15th and 16th centuries. It was finally reduced to a village in 1580 by the Ural Cossacks.

After the Russian conquest of the Ural basin in the late 16th century, the shores of the Ural became home to the Yaik Cossacks. One of their main activities was fishing for the sturgeon and related fishes (including the true sturgeon, starry sturgeon, and beluga) in the Ural River and the Caspian. A great variety of fishing techniques existed; the most famous of them was ''bagrenye'' (, from ''bagor'' , meaning pike pole): spearing hibernating sturgeons in their underwater lairs in mid-winter. The ''bagrenye'' was allowed only on one day of the year. On the appointed day, a large number of Cossacks with pike poles were gathering on the shore; after a signal was given, they rushed on the ice, broke it with their poles, and speared and pulled the fish. Another fishing technique was constructing a weir, known as the ''uchug'' ( учуг) across the river, to catch fish going upstream to spawn. Until 1918, an ''uchug'' was set up in the summer and autumn near Uralsk, so that the fish would not go upstream beyond the Cossacks' land. While the ''uchug'' weirs were also known in the Volga Delta, the ''bagrenye'' was thought to be a uniquely Ural technique.

The Ural Cossacks (known originally as the Yaik Cossacks) resented the attempts by the central government to impose rules and regulations on them, and on occasions rose in rebellions. The largest rebellion, the Pugachev's Rebellion of 1773–75, involved not only the Ural, but much of south-eastern Russia, and resulted in a loss of the government control there. After its suppression, Empress Catherine issued a decree of 15 January 1775 to rename most of the places involved in the revolt, in order to erase the memory of it. Thus the Yaik River and the city of Yaitsk were renamed to the Ural River and Uralsk, respectively, and the Yaik Cossacks became the Ural Cossacks.

On 6 April 2024, during the Snowmelt, a levee sheltering the city of Orsk broke. A flood in Orenburg set over 10,000 houses under water, and parts of Kazakhstan were also concerned.

Geography

The river begins on the slopes of the Kruglaya MountainUral River
Encyclopædia Britannica of the Uraltau mountain ridge in South Ural, on the territory of the Uchalinsky District of Bashkortostan. There it has an average width of and flows as a typical mountain river. It then falls into the Yaik Swamp and after exiting it widens up to . Below Verkhneuralsk, its flow is characteristic of a flatland river; there it enters Chelyabinsk and Orenburg Oblasts. From Magnitogorsk to Orsk its banks are steep and rocky and the bottom has many rifts. After Orsk, the river abruptly turns west and flows through a long canyon in the Guberlinsk Mountains. After Uralsk, it flows from north to south, through the territory of West Kazakhstan Region and Atyrau Region of Kazakhstan. There, the river widens and has many lakes and ducts. Near the mouth, it splits into the Yaik and Zolotoy distributariesV. A. Balkov
Ural
(in Russian). bashedu.ru and forms vast wetlands. The Yaik distributary is shallow, with almost no trees on the shores, and is rich in fish; whereas Zolotoy is deeper and is navigable. Ural River has a spectacular tree-like (or "digitate") shape of the delta (see image). This type of delta forms naturally in the slow rivers which deliver a great deal of sediments and flow into a quiet sea. In the delta, from the mouth of the Zolotoy distributary lies Shalyga Island, which is long, with heights of and maximum widths of .

The tributaries, in order going upstream, are Kushum, Derkul, Chagan, Irtek, Utva, Ilek (major, left), Bolshaya Khobda, Kindel, Sakmara, Tanalyk (major, right), Salmys, Or (major, left) and Suunduk. The Kushum and Bagyrlai are distributaries.

The entire length of the Ural River is considered the Europe-Asia boundary by most authoritative sources. "Europe" (plate 59); "Asia" (plate 74): "A commonly accepted division between Asia and Europe ... is formed by the Ural Mountains, Ural River, Caspian Sea, Caucasus Mountains, and the Black Sea with its outlets, the Bosporus and Dardanelles." Rarely, the smaller, shorter Emba River. The Ural River bridge in Orenburg is even labeled with permanent monuments carved with the word "Europe" on one side, "Asia" on the other. Regardless, Kazakhstan has some European territory and is at times included in European political and sports organizations.

Hydrography

The river is mostly fed by melting snow (60–70%); the contribution of precipitation is relatively minor. Most of its annual discharge (65%) occurs during the spring floods, which occur in March and April near the mouth and in late April through June upstream; 30% drain during the summer and autumn and 5% in winter. During the floods, the river widens to above near Uralsk and to several tens of kilometers near the mouth. Water level is highest in later April upstream and in May downstream. Its fluctuation is in the upper stream, in the middle of the river and about in the delta. The average water discharge is near Orenburg, and at the Kushum village, which is from the mouth. The maximum discharge is and the minimum is . Average turbidity is at Orenburg and near Kushum. The river freezes at the source in early November and in the middle and lower reaches in late November. It opens in the lower reaches in late March and in early April in the upper reaches. The ice drift is relatively short.

The average depth is near the source, and it increases in the middle reaches and especially near the mouth. The density of underwater vegetation also increases from the source to the mouth, so does the richness of the fauna. The bottom in the upper stream is rocky, with pebble and sand; it changes to silt-sand and occasionally clay downstream. The basin is asymmetrical – its left side from the river is 2.1 times larger in area than the right side; however, the right side is more important for feeding the river. The density of the tributaries is 0.29 km/km² in the right and 0.19 km/km² in the left side of the basin. The right-side tributaries are typical mountain rivers whereas the left-side tributaries have flatland character. About from the mouth there is a dangerous spot for shipping called Kruglovskaya prorva ( meaning Kruglovsk abyss). Here the river narrows and creates a strong vortex over a deep pit. The climate is continental with frequent and strong winds. Typical annual precipitation is .800 km on Ural River
(in Russian)Ural River
chelindustry.ru (in Russian)

Fauna

The wetlands at and near the delta of the Ural River are especially important to migrating birds as an important stop-over along the Asian flyway. They host many endemic and endangered species, such as great white pelican, Dalmatian pelican, pygmy cormorant, cattle egret, little egret, greater flamingo, white-headed duck, ferruginous duck, Eurasian spoonbill, glossy ibis, houbara bustard, great black-headed gull, slender-billed gull, squacco heron, common crane, demoiselle crane, slender-billed curlew, black stork, red-breasted goose, lesser white-fronted goose, lesser kestrel, whooper swan, tundra swan, osprey, pallid harrier, short-toed eagle and many others. The pygmy cormorant was observed sporadically before 1999 and more regularly after that. Cattle egret is observed since 1990 between April and September (as most other migratory birds in this area), with the total population of several dozen couples. It feeds on frogs, mollusks and small fish.Фауна: Дельта реки Урал и прилегающее побережье Каспийского моря
wetlands.kz. (Fauna of the delta of Ural River, in Russian) Upstream, there are more of the resident bird species, such as grouse, wild pigeon and partridge.

Ural River is also important for many fish species of the Caspian Sea which visit its delta and migrate upstream for spawning. In the lower reaches of the river there are 47 species from 13 families. The family Cyprinidae account for 40%, sturgeon and herring make up 11%, perch and herring 9% and salmon 4.4%. The main commercial species are sturgeon, roach, bream, perch, carp, asp and Wels catfish. The rare species include Caspian salmon, sterlet, white salmon and kutum.

In the delta of the river and nearby regions live about 48 animal species belonging to 7 orders; most common are rodents (21 species) and predators (12). Among them, Bobrinski's serotine and marbled polecat are endemic. Key species are raccoon dog, muskrat (appeared recently), European hare, house mouse, brown rat, and wild boar. Wild boars had a density of 1.2–2.5 per hectare in 2000 and are hunted commercially. Others include elk, fox, wolf, dwarf fat-tailed jerboa, great gerbil, northern mole vole and saiga antelope. The Turkmenian kulan (''Equus hemionus kulan'') used to live at the Ural River. It might be extinct from that region.

The reptiles are represented by bog turtles, common water snakes, rat snakes and sand lizard. Bog turtles are found in all waters. Common water snakes live on the banks of canals. Rat snakes and sand lizards are few and inhabit relatively high areas of land. Two more reptiles, Caspian whipsnake and '' Coluber spinalis'', are extremely rare. Among amphibians common are lake frog and green frog.

With an estimated 5,000 to 10,000 species, insects exceed all other animals of the region by diversity and biomass. Terrestrial and aquatic insects make up a significant proportion of the diet of birds. Many species are parasitic on birds and transmit infection. Other dominating inhabitants of the river are protozoa, rotifers, Cladocera and copepods. Mollusks are mostly represented by gastropods and bivalves.

File:Loeffler.jpg, Eurasian spoonbill
File:Ellobius talpinus.jpg, Northern mole vole
File:Rhombomys opimus 1.jpg, Great gerbil
File:Marbled polecat.jpg, Marbled polecat
File:Sturgeon.jpg, Sturgeon

Industry

Water from the upper reaches of the Ural River is used to supply the prominent Magnitogorsk ( Magnitogorsk Iron and Steel Works, built in the early 1930s) and Orsk-Khalilovsk metallurgical plants, and the low reaches are used for irrigation. Two reservoirs were created near Magnitogorsk, and there is a hydroelectric plant near the village of Iriklinskaya with the corresponding reservoir. Below Uralsk, there is another reservoir and the Kushumsky channel. The river is navigated up to Uralsk and there is a port in Atyrau.Zonn, p. 45 Fishery is well developed; the commercial fish species include sturgeon, perch, herring, bream, carp and catfish. The delta of Ural River accounts for about half of the fish catchment in Kazakhstan. Also widespread is agriculture, especially growth of melons and watermelons. The city of Atyrau is a major oil producing center of Kazakhstan.

See also

* Boundaries between the continents
* Ural Mountains

Notes

References

Bibliography

*

{{Authority control

Rivers of Kazakhstan
Rivers of Russia
Tributaries of the Caspian Sea
Rivers of Chelyabinsk Oblast
Rivers of Bashkortostan
Rivers of Orenburg Oblast
Border rivers
International rivers of Asia
International rivers of Europe
Ural Mountains
History of Ural