Kura (South Caucasus river)

Coordinates: 40°40′18″N 42°45′55″E / 40.6715688305°N 42.765199064°E / 40.6715688305; 42.765199064
Source: Wikipedia, the free encyclopedia.
This article is about the river in the South Caucasus. For the river in North Caucasus, see Kura (Russia). For other uses, see Kura (disambiguation).
Kura
Kür, Mtkvari (Georgian: მტკვარი)
Zardab
  • Sabirabad
  • Neftçala
    • Physical characteristics
    SourceLesser Caucasus
     • locationNear Kartsakhi Lake, Kars, Turkey
     • coordinates40°40′31″N 42°44′32″E / 40.67528°N 42.74222°E / 40.67528; 42.74222
     • elevation2,740 m (8,990 ft)[4]
    Neftchala Rayon, Azerbaijan
     • coordinates
    		40°40′18″N 42°45′55″E / 40.6715688305°N 42.765199064°E / 40.6715688305; 42.765199064 40.67156883058258, 42.76519906444574
     • elevation
    		−26.5 m (−87 ft)[5]
    Length1,515 km (941 mi)[1]
    Basin size198,300 km2 (76,600 sq mi)[6]
    Discharge 
     • locationdirectly downstream from Aras River confluence[2]
     • average443 m3/s (15,600 cu ft/s)[2]
     • minimum206 m3/s (7,300 cu ft/s)[3]
     • maximum2,250 m3/s (79,000 cu ft/s)[3]
    Discharge 
     • locationborder of Georgia and Azerbaijan
     • average378 m3/s (13,300 cu ft/s)
    Basin features
    Tartarchay, Aras

    The Kura, also known in Georgian as Mtkvari (Georgian: მტკვარი, romanized: mt'k'vari [ˈmt'k'ʷäɾi]), is an east-flowing transboundary river south of the Greater Caucasus Mountains which drains the southern slopes of the Greater Caucasus east into the Caspian Sea. It also drains the north side of the Lesser Caucasus, while its main tributary, the Aras, drains the south side of those mountains. Starting in northeastern Turkey, the Kura flows through to Georgia, then into Azerbaijan, where it receives the Aras as a right tributary, and finally enters the Caspian Sea. The total length of the river is 1,515 kilometres (941 mi).

    People have inhabited the Caucasus region for thousands of years and first established

    hydroelectric power stations. The river is now moderately polluted by major industrial centers like Tbilisi and Rustavi
    in Georgia.

    Etymology

    The name Kura is related either to

    Megrelian tkvar-ua "gnaw" (as in, "river that eats its way through the mountains").[7] The name Kura was adopted first by the Russians and later by European cartographers. In some definitions of Europe, the Kura defines the borderline between Europe and Asia.[8]

    In the various regional languages, the river is known as:

    Latin: Cyrus, as attested by Strabo and Pliny respectively.[9] Bundahishn, a Zoroastrian source written in Book Pahlavi, refers to the river as Tord in Persian.[12]

    The river should not be confused with the Kura river in Russia, a westward flowing tributary of the Malka in Stavropol Krai; the Kur near Kursk, Russia; Kur near Khabarovsk, also in Russia and Kor River, which is located in Fars province, Iran.

    Course

    Old map showing the drainage south of the Caucasus split between the Phasis on the west and the Kura on the east

    It rises in northeastern

    Shemkir reservoir and then Yenikend reservoir.[14]

    The Kura then empties into

    irrigated plain for several hundred kilometers, turning east near Lake Sarysu, and shortly after, receives the Aras, the largest tributary, at the city of Sabirabad. At the Aras confluence it makes a large arc to the north and then flows almost due south for about 60 kilometres (37 mi), passing the west side of Shirvan National Park, before turning east and emptying into the Caspian Sea at Neftçala.[14]

    Basin

    Kura making its way through mountains, as viewed from the walls of Atskuri Fortress in Georgia.

    Most of the Kura runs in the broad and deep valley between the Greater Caucasus and Lesser Caucasus Mountains, and the major tributary, the Aras, drains most of the southern Caucasus and the mountain ranges of the extreme northern Middle East. The entirety of Armenia and most of Azerbaijan are drained by the river. Most of the elevation change in the river occurs within the first 200 kilometres (120 mi). While the river starts at 2,740 metres (8,990 ft) above sea level, the elevation is 693 metres (2,274 ft)[15] by the time it reaches Khashuri in central Georgia, just out of the mountains, and only 291 metres (955 ft)[15] when it reaches Azerbaijan.

    The Kura (Mtkvari) near Gori, Georgia

    The lower part of the river flows through the

    Kura-Aras Lowland, which covers most of central Azerbaijan and abuts the Caspian Sea. The Kura is the third largest, after the Volga and Ural, of the rivers that flow into the Caspian. Its delta is the fourth largest among the rivers that flow into the Caspian Sea,[2] and is divided into three main sections, or "sleeves", composed of sediment the river deposited during different periods of time. Before 1998, the river flowed all the way to the tip of the delta, where it discharged into the Caspian. In that year, the river escaped its channel and started to flow off to the west, leaving the last few kilometers abandoned. The course change is believed to be the result of a rise in the level of the Caspian Sea coupled with a major flood of the Kura.[16]

    About 174 kilometres (108 mi) of the river is in Turkey, 435 kilometres (270 mi) in Georgia, and 906 kilometres (563 mi) in Azerbaijan.[13][17] About 5,500 square kilometres (2,100 sq mi) of the catchment is in Turkey, 29,743 square kilometres (11,484 sq mi) in Armenia,[18] 46,237 square kilometres (17,852 sq mi) in Georgia, 56,290 square kilometres (21,730 sq mi) in Azerbaijan,[19] and about 63,500 square kilometres (24,500 sq mi) are in Iran. At the confluence with the Aras River, the drainage area of the tributary is actually larger than the Kura by about 4%, and it is also longer.[17][20] However, because of the more arid conditions and equally intensive water use, the discharge of the Aras is much less than the Kura, so downstream of the confluence the river is still called the Kura. About 52% of the river's flow comes from snowmelt and glaciers, 30% comes from groundwater seepage, and roughly 18% from precipitation.[17] Because of high water use, many of the smaller tributaries of the Kura no longer reach the river, instead disappearing in the plain many kilometers from their original mouths.[17]

    Tributaries

    The following rivers are tributaries of the Kura, from source to mouth:

    Ecology

    The Kura flowing along the Metekhi neighborhood of Tbilisi, Georgia

    nase, and many of these fish are endemic to the region. Among rivers of the Caucasus, the Kura has the largest number of endemic species. The upper section of the river supports much more biodiversity than the lower half, which is typically more turbid and polluted. This pattern is also apparent in most of its tributaries, especially the larger ones that span more climate zones, such as the Aras and Alazani. There are many lakes and wetlands along the Kura's lower course, most of which are formed by flooding, and some of which are formed by irrigation runoff water. Many lakes also form at the mouths of small tributaries that do not reach the ultimate destination in the Caspian most of the time. The local name for these lakes translate to dead lake or dead water, suggesting that these lakes do not support much biodiversity.[21]

    Economy and human use

    Formerly navigable up to

    dikes and dams, the largest of which is at Mingachevir, an 80-metre (260 ft)-high rockfill dam impounding over 15.73 cubic kilometres (12,750,000 acre⋅ft) of water.[20] However, because of the high sediment content of rivers in the Kura basin,[2]
    the effectiveness of these floodworks is limited and decreases every year.

    Irrigation agriculture has been one of the primary economic mainstays of the lower Kura valley since ancient times.[22] Because of water taken out for irrigation use, up to 20% of the water that formerly flowed in the river no longer reaches the Caspian Sea. Over 70% of the water in the Iori (Gabirry) River, a major tributary of the Kura, is expended before it reaches Lake Mingachevir.[17] Of the 4,525,000 hectares (11,180,000 acres) of agricultural land in the lower Kura catchment area, 1,426,000 hectares (3,520,000 acres), about 31%, are irrigated.[22] Much of the water diverted from the river for irrigation goes to waste because of leakage from the canals, evaporation, poor maintenance, and other causes. Leaking water causes groundwater to rise, in some areas so high that about 267,000 hectares (660,000 acres) of land are so waterlogged that they are no longer suitable for agriculture. About 631,000 hectares (1,560,000 acres) of the irrigated lands have a dangerously high salt content because of mineral deposits from irrigation. Of this, 66,000 hectares (160,000 acres) are extremely salinated. Irrigation returns water, returned to the river by an extensive but outdated[22] drainage system, contributes to severe pollution. Some of this degradation also comes from industrial and municipal wastewater discharge.[1]

    History

    Kura in Azerbaijan

    The ancient inhabitants of the Kura-Aras lowland called the river Mother Kür, signifying the importance of the river to the region.[6] The first irrigation agriculture began about 4,500 years ago in the eastern Azerbaijan lowlands. Trading centers were established in time, including one at Mingachevir in Azerbaijan and another at Mtskheta in Georgia.

    The site at Mingachevir (probably Sudagylan

    archaeologist G. I. Ione, had "seven rectangular kilns ... The fuel chamber was a trapezoid. The inner walls and floor were covered with a special coating. These kilns were attributed to the third century B.C. [2,300 years ago]. The number of kilns and the quantity of raw material indicate a trade center."[24] The settlement was probably destroyed by a fire around A.D. 600, but its demise is uncertain.[23] But perhaps the most famous of the ancient settlements on the Kura is the "cave town" at Uplistsikhe, Georgia, first settled as early as 3,500 years ago. The city, carved into a cliff on the bank of the Kura covering an area of 8 hectares (20 acres), contains underground living quarters, communal chambers, places of worship, storerooms, connected by a network of passageways. It reached its peak about 1,100 years ago as the political, religious and cultural center of the region, but in the 13th century, it fell to Mongolian invaders.[25]

    Kura (Mtkvari) near Gori, Georgia

    Even though irrigation agriculture had been well established for thousands of years, until the 1920s, humans did not have a significant effect on the ecology or hydrology of the Kura catchment area. Since then,

    wetlands were drained and reservoirs were created to facilitate development of irrigation in the lower Kura valley.[26]

    In the 1950s and 1960s, when the Caucasus region was part of the Soviet Union, construction of many of the reservoirs and waterworks in the Kura basin began. Of the major reservoirs in the Kura catchment, one of the earliest was at Varvara in 1952. Large-scale construction of dams continued until the 1970s.[6][22]

    See also

    References

    1. ^ a b "Regional Partnership for Prevention of Transboundary Degradation of the Kura-Aras River Basin". Environmental Conservation and Management. United Nations Development Programme. 2002. Archived from the original on November 20, 2008. Retrieved 2010-03-12.
    2. ^ a b c d Rustanov, S. G. (1967). "Drift Balance of the Kura River in its Lower Course" (PDF). Institute of Geography of the Academy of Sciences of the Azerbaijan SSR. Symposium on River Morphology. General Assembly of Bern. Commission of Surface Waters. Retrieved 2010-04-05.
    3. ^ a b "Kura River Discharge at Surra". River Discharge Database. Center for Sustainability and the Global Environment. 1930–1984. Archived from the original on 2010-06-16. Retrieved 2010-03-12.
    4. ^ Guluzada, Lidiya. "Kura River—Transboundary Watercourse of Caucasus" (PDF). Fondazione Eni Enrico Mattei. Retrieved 2010-03-12.
    5. ^ "General Background". Caspian Environment Programme. 2004-11-06. Archived from the original on 2001-04-14. Retrieved 2010-03-12.
    6. ^ a b c d Mammadov, R.M.; Verdiyev, R. (February 2009). "Integrated Water Resources Management as Basis for Flood Prevention in the Kura River Basin" (PDF). United Nations Economic Commission for Europe. Retrieved 2010-03-12.
    7. ^ Pospelov, E.M. Geograficheskie nazvaniya mira (Moskva, 1998), p. 231.
    8. ^ "Countries that exist wholly or partially within geographical Europe". Archived from the original on 2018-05-23. Retrieved 2011-12-03.
    9. ^ a b c Wordsworth, Paul (2021). "KURA RIVER". In Yarshater, Ehsan (ed.). Encyclopædia Iranica (Online ed.). Encyclopædia Iranica Foundation.
    10. ISBN 978-0-7100-6959-7
    11. ISBN 978-0-89096-703-4
    12. ISSN 1573-384X
      .
    13. ^ a b "Azerbaijan: Geography, climate and population". AQUASTAT. Food and Agriculture Organization of the United Nations. Archived from the original on 2010-06-19. Retrieved 2010-03-18.
    14. ^ a b Megvinetukhutsest, Nutsa. Background Map of the Kura-Aras River Basin (PDF) (Map). Cartography by Trans-Boundary River Management Phase II for the Kura River basin—Armenia, Georgia, Azerbaijan. European Union. Archived from the original (PDF) on 2010-10-13. Retrieved 2010-03-12.
    15. ^ a b Derived from Google Earth
    16. ^ Mamedova, N. "Using Spaceborne Data and GIS-technology for Research of Coastal Zone in Azerbaijan" (PDF). Department of General Geography, Baku State University, Azerbaijan. International Society for Photogrammetry and Remote Sensing. Archived from the original (PDF) on 2011-07-17. Retrieved 2010-03-13.
    17. ^ a b c d e Mustafaev, Islam; Mammadov, Vagif. "Problems of Transboundary Water Management in Azerbaijan". Institute of Radiation Problems, Institute of Geology. docstoc. Retrieved 2010-03-13.
    18. ^ Armenia is entirely in the Kura River catchment
    19. ^ Problems of Transboundary Water Management in Azerbaijan report states that 65% of Azerbaijan is drained by the Kura
    20. ^ a b Mammadov, R.; Ismatova, Kh.; Verdiyev, R. "Integrated Water Resources Management As Basis for Flood Prevention in the Kura River Basin" (PDF). Azerbaijan Geographical Society, Azerbaijan Aerospace Agency. Retrieved 2010-03-12.
    21. ^ Bogutskaya, Nina (2010-03-11). "Kura-South Caspian Drainages". World Wildlife Fund, Nature Conservancy. Freshwater Ecoregions of the World. Archived from the original on 2011-10-05. Retrieved 2010-03-18.
    22. ^ a b c d Imanov, Farda A. "Water Infrastructure of Kura River Basin Within Azerbaijan" (PDF). Basin Resources Protection. General Directorate of State Hydraulic Works. pp. 100–105. Archived from the original (PDF) on 2016-10-20. Retrieved 2010-03-12.
    23. ^ a b Pasichnyk, Richard Michael (2009-05-02). "AD 550 to 750—A Time for the New World's Renewal and Being 'Gracious to the Creatures' – Another Example of a Historical Cycle". Living Cosmos. Archived from the original on 2009-12-17. Retrieved 2010-03-13.
    24. S2CID 191409715
      .
    25. ^ "Uplistsikhe Cave Town". UNESCO World Heritage Center. United Nations. 2007-10-24. Retrieved 2010-03-13.
    26. ISBN 0-521-36357-8
      .
    • Media related to Kura River at Wikimedia Commons
    • Kura.
      The Columbia Encyclopedia
      , Sixth Edition. 2001–05.
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