Kura (South Caucasus river)

Kura
Mtkvari
Confluence of clay-colored waters of Kura (left) with Aragvi (right) near Mtskheta
Kura River Basin
Location
Countries
RegionCaucasus
Cities
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)[1]
MouthCaspian Sea
 • location
Neftçala, 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)[2]
Length1,515 km (941 mi)[3]
Basin size198,300 km2 (76,600 sq mi)[4]
Discharge 
 • locationdirectly downstream from Aras River confluence[5]
 • average443 m3/s (15,600 cu ft/s)[5]
 • minimum206 m3/s (7,300 cu ft/s)[6]
 • maximum2,250 m3/s (79,000 cu ft/s)[6]
Discharge 
 • locationborder of Georgia and Azerbaijan
 • average378 m3/s (13,300 cu ft/s)
Basin features
River systemCaspian Sea basin
Tributaries 
 • leftLiakhvi, Ksani, Aragvi, Iori, Alazani
 • rightAlgeti, Khrami, Tartarchay, Aras
Map

The Kura, also known in Georgian as Mtkvari, 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 agriculture in the Kura Valley over 4,500 years ago. Large, complex civilizations eventually grew on the river, but by 1200 CE most were reduced to ruin by natural disasters and foreign invaders. The increasing human use, and eventual damage, of the watershed's forests and grasslands, contributed to a rising intensity of floods through the 20th century. In the 1950s, the Soviet Union started building many dams and canals on the river. Previously navigable up to Tbilisi in Georgia, the Kura is now much slower and shallower, having been harnessed by irrigation projects and hydroelectric power stations. The river is now moderately polluted by major industrial centers like Tbilisi and Rustavi in Georgia.

  1. ^ Guluzada, Lidiya. "Kura River—Transboundary Watercourse of Caucasus" (PDF). Fondazione Eni Enrico Mattei. Retrieved 2010-03-12.
  2. ^ "General Background". Caspian Environment Programme. 2004-11-06. Archived from the original on 2001-04-14. Retrieved 2010-03-12.{{cite web}}: CS1 maint: unfit URL (link)
  3. ^ Cite error: The named reference UNDP was invoked but never defined (see the help page).
  4. ^ Cite error: The named reference overview was invoked but never defined (see the help page).
  5. ^ a b Cite error: The named reference sediment was invoked but never defined (see the help page).
  6. ^ 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.

Kura (South Caucasus river)

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