Река Кура: География и гидрография региона Кавказа.

River in the Caucasus region
the river south of the Caucasus
40.67156883058258, 42.76519906444574
| mouth elevation =
| progression =
| river system = Caspian Sea basin
| basin size = 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. In the various regional languages, the river is known as: , , Mt’k’vari, Persian: Korr,, Kour, and Kür. Cyrus, as attested by Strabo and Pliny respectively. 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.

It rises in northeastern Turkey in a small valley in the Kars Upland of the Lesser Caucasus. It flows west, then north and east past Ardahan, and crosses into Georgia. It arcs to the northwest, then into a canyon near Akhaltsikhe where it starts to run northeast in a gorge for about , spilling out of the mountains near Khashuri. It then arcs east before flowing east southeast for about , past Gori, then near Mtskheta, flows south through a short canyon and along the west side of T'bilisi, the largest city in the region. The river flows steeply southeast past Rustavi and turns eastward at its confluence with the Khrami, crossing the Georgia Azerbaijan border and flowing across grasslands into Shemkir reservoir and then Yenikend reservoir. The Kura then empties into Mingachevir reservoir, the largest body of water in Azerbaijan, formed by a dam near its namesake town at the southeastern end. The rivers Iori (also known as Qabirri) and Alazani formerly joined the Kura, but their mouths are now submerged under the lake. After leaving the dam, the river meanders southeast where it meets its biggest tributary Tartarchay in Barda Rayon and continues across a broad 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 , passing the west side of Shirvan National Park, before turning east and emptying into the Caspian Sea at Neftçala. by the time it reaches Khashuri in central Georgia, just out of the mountains, and only 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. About of the river is in Turkey, in Georgia, and in Azerbaijan. About of the catchment is in Turkey, in Armenia, in Georgia, in Azerbaijan, and about 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. 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.

Formerly navigable up to Tbilisi, the largest city on the river, the amount of water in the Kura has greatly diminished in the 20th century because of extensive use for irrigation, municipal water, and hydroelectricity generation. The Kura is regarded as one of the most stressed river basins in Asia. Most of the water comes from snowmelt and infrequent precipitation in the mountains, which leads to severe floods and an abundance of water for a short time of the year (generally in June and July), and a relatively low sustainable baseflow. Forest cover is sparse, especially in the Kura and Aras headwaters, and most of the water that falls on the highlands becomes runoff instead of supplying groundwater. Attempts at flood control include the constructions of levees, dikes and dams, the largest of which is at Mingachevir, an high rockfill dam impounding over of water. 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.

People have lived on the Kura for at least 7,000 years. The ancient inhabitants of the Kura Aras lowland called the river Mother Kür, signifying the importance of the river to the region. ), first discovered in the 1940s by 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." The settlement was probably destroyed by a fire around A. D. 600, but its demise is uncertain. 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, logging, grazing and especially agriculture began to have a severe outcome on the water availability of the basin. Many forested areas in the mountains have been replaced by thin grassland because of logging. These habitat changes have been detrimental to the ecology of the Kura basin. After the 1920s, wetlands were drained and reservoirs were created to facilitate development of irrigation in the lower Kura valley. 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.