The Kaveri (anglicized as Cauvery), historically known in Tamil as Ponni (), is a major river flowing across southern India. It is the third-largest river in the peninsula after the Godavari and Krishna. The river basin covers an estimated catchment area of , across the states of Tamil Nadu, Karnataka, Kerala, and the Union Territory of Puducherry.
The river rises at Talakaveri in the Brahmagiri range of the Western Ghats, at an elevation of in the Kodagu district of Karnataka. It traverses approximately across the Deccan Plateau in Karnataka before entering Tamil Nadu, flowing a further eastward to empty into the Bay of Bengal near Poompuhar in Mayiladuthurai district. Over its total course of roughly , major tributaries include Harangi, Hemavati, Lakshmana Tirtha, Kabini, Shimsha, Arkavati, Bhavani, Noyyal, and Amaravati.
Multiple dams and reservoirs along the river support regional irrigation systems and hydroelectric power generation. The river has supported agriculture in the region for centuries and historically supported early agricultural states, including the Chola and Pandya kingdoms. Sharing of its waters has been a long-standing Kaveri River water dispute between Karnataka and Tamil Nadu. The Kaveri River basin is a densely populated region, with several towns and cities located on its banks.
In Hinduism, the Kaveri is revered as one of the seven sacred rivers (Sapta Sindhu) and is personified as the goddess Kaveriamma. It is praised in Sanskrit epics including the Mahabharata and various Puranas, as well as throughout classical Sangam literature.
Etymology Kaveri is mentioned in Sanskrit literature, including the Mahabharata and the Puranas, as a sacred river. The name itself might have had different etymologies. According to a legend in the Skanda Purana, the river originated when Ganesha, in the guise of a crow, overturned sage Agastya's kamandala (water vessel). Linguistically, the name Kaveri has been derived from Dravidian roots, such as the Kannada terms ಕಾವಿ (Kāvi): Red ochre, saffron, or reddish-brown clay and ಏರಿ (Ēri): A watercourse, bank, bund, or elevated stream channel. An alternative derivation links it to viri (to spread out or wide banks). The term kāviri alos occurs in the Sankethi dialect to denote a river. The spelling Cauvery is an anglicization done during the colonial period.
In classical Tamil literature, the river is frequently called Ponni (meaning "the golden one"), in reference to the gold-colored fertile silt it deposited along its delta during floods. In Sanskrit traditions, it is also known as Daksina Gaṅgā (Ganges of the South), and Ardha Gaṅgā (Half Ganga) due to its mythological association with the celestial Ganges. Some scholars also identify it with the Rigvedic river name Marudvṛdhā (rejoicing with the Maruts).
Course
The river rises at Talakaveri in the Brahmagiri Hills of the Western Ghats, located at an elevation of in the Kodagu district of Karnataka. Its upper course passes through rocky terrains and steep banks before flowing eastward through a series of rapid falls. Flowing onto the Deccan Plateau through a narrow gorge, the river drops about at Chunchanakatte Falls. It then forms the river island of Srirangapatna and widens to before turning south-east. At Shivanasamudra, it drops to form the Shivanasamudra Falls, one of the largest waterfalls in the country. After forming the island of Shivanasamudra, the river converges and passes through the Mekedatu gorge. After traversing within Karnataka, the river forms the Karnataka–Tamil Nadu border for roughly .
Upon entering Tamil Nadu, the river forms the Hogenakkal Falls, before continuing south toward the Mettur Dam, where it is joined on its right bank by River Bhavani at Kooduthurai. Flowing eastward through Erode and Karur, it enters Tiruchirappalli district and bifurcates into northern Kollidam and southern Kaveri. The two branches form the river island Srirangam before diverging across an extensive delta of 36 distribution channels. It ultimately discharges into the Bay of Bengal near Poompuhar in Mayiladuthurai district. The river traverses for about in Tamil Nadu, bringing its total length to approximately .
Tributaries The Kaveri River has 21 major tributaries. In Karnataka, major tributaries include the Hemavati, Lakshmana Tirtha and Kabini, with the former two joining at Krishna Raja Sagara reservoir. The Shimsha and Arkavati enter before the river reaches Tamil Nadu, where it receives Bhavani at Kooduthurai, followed downstream by Noyyal, Amaravati, Sarabanga, and Thirumanimutharu.
Discharge Source: +DischargeYearGrand AnicutLower Anicut (m3/s)(m3/s)MinMeanMaxMinMeanMax19981701,0993,4541618852,54019992891,1313,7782858642,84520003431,2874,9032331,0113,33520012581,0803,3483099483,11520021397722,3921448672,4232003786672,2972166462,10020041038953,3032178393,16020051791,0123,3542409913,87320062681,0722,4954731,0913,18720071189933,3083241,1264,07520081321,0943,6773981,1033,16720092271,0403,2382909653,30120103731,0803,1414111,0223,62620111711,1633,8152969283,01420121908743,3421777112,1492013821,0433,2812298563,12720142791,1483,6634099802,53320155591,4223,8164079132,17720164901,1292,8902767281,73320172169313,5861546711,83220183411,5714,4392669343,42720193311,4734,5591739663,07020205911,5904,3732099832,94420214781,5023,9352579883,13620225481,7134,9164071,1723,385Overall781,1514,9161449284,075
Geology and ecology
The Kaveri basin was formed between the Late Jurassic and Early Cretaceous periods during the breakup of Gondwana and the opening of the Indian Ocean. Most of the basin is underlain by Precambrian metamorphic and igneous basement rocks. Closepet Granite is found in the upper catchment, while charnockite rocks are found in the central basin. A 2017 study proposed that presence of putative meteorite impact structure in the vicinity of the basin. The basin's topography prevents rapid run-off, reducing the frequency of flash floods. The river maintains perennial flow supported by dual monsoon cycles: the southwest monsoon in Karnataka and the northeast monsoon in Tamil Nadu.
According to a 2014–15 government assessment, the basin generates nearly 3.5 million metric tons of dissolved salts annually, with an average salinity of 441 ppm, close to the standard maximum limit of 500 ppm. Increased population density and agricultural runoff have increased salt inputs, while salt export is hindered by reduced fresh water discharge to the sea. This degrades basin water quality.
The basin encompasses forest and agro–ecological zones, with forest types ranging from moist evergreen and dry deciduous forests to grasslands. A remote-sensing study found that approximately of natural vegetation was lost in the basin between 1965 and 2016. Regional flora includes species such as Terminalia arjuna, Tamarindus indica, Pongamia pinnata, Salix tetrasperma, Ficus benghalensis, Ficus religiosa, Eucalyptus torticornis, and Diospyros montana.
The basin contains several protected areas that support populations of Bengal tiger, Indian elephant, gaur, leopard, sloth bear, Nilgiri tahr and grizzled giant squirrel apart from various species of deer, wild boar and reptiles. Avifauna includes the painted stork (Mycteria leucocephala), spot-billed pelican (Pelecanus philippensis), and black-headed ibis (Threskiornis melanocephalus). Aquatic wildlife includes the mugger crocodile (Crocodylus palustris), smooth-coated otter (Lutrogale perspicillata), and the critically endangered hump-backed mahseer (Tor remadevii).
Dams and flow regulation structures have fragmented the longitudinal and lateral connectivity of the river, disrupting aquatic habitats and migratory fish routes. The reduction of sediment, nutrient, and freshwater delivery has impacted estuarine ecosystem in the delta. Reduced stream flows and suppressed natural flow pulses have caused steep declines in migratory fish populations. Seasonal low-flow conditions threaten the survival of the endemic and endangered hump-backed mahseer.
Riparian zone
The Kaveri basin covers a total catchment area of , comprising in Tamil Nadu, in Karnataka, in Kerala, and in the Union Territory of Puducherry. Over half of the basin is arable land, with rice and sugarcane being the primary crops. During the first Five-Year Plan, the total flow of the river was estimated at , of which approximately 60% was utilized for irrigation. The river also provides drinking water and supports hydroelectric power generation.
Dams About 96 dams have been built across the Kaveri basin over the past millennium, most of which are small-scale barrages and weirs. Irrigation is the primary function for 70.30% of these structures, followed by hydroelectric power generation (19.80%), combined irrigation and power (6.93%), and municipal drinking water supply (2.97%).
The ancient Grand Anicut (Kallanai) was constructed during the early Chola period in the 2nd century CE. Modern infrastructure began with the Shivanasamudra hydroelectric installation in 1902, one of the earliest major hydroelectric plants in Asia. In Tamil Nadu, the Mettur Dam was completed in 1934 forming the Stanley Reservoir with a gross storage capacity of 93.4 tmc ft (2.64 km3). In Karnataka, the Krishna Raja Sagara dam, completed in 1938, is the second-largest reservoir on the river with a capacity of 49.5 tmc ft (1.40 km3). Principal tributary storage projects include the Bhavanisagar Dam (32.8 tmc ft) on the Bhavani River in Tamil Nadu, as well as the Gorur dam (37.1 tmc ft) on the Hemavathi, the Kabini Dam (18.5 tmc ft) on the Kabini, and the Harangi Dam (9.5 tmc ft) on the Harangi in Karnataka. Although these rivers expanded the basin's irrigation coverage, water retention has aggravated political disputes over water sharing between upstream and downstream states.
Hydrological alterations Hydrological modelling shows that reservoir operations have altered Kaveri's natural flow across all major sub-basins. Monsoon storage has caused year-round decline in monthly median flows and suppressed seasonal peak floods. Moreover, irrigation storage has extended downstream low-flow periods, while hydroelectric power projects such as Kabini produce fluctuations in flow due to short-term peak releases.
Water sharing dispute
Historical agreements and interim award
The dispute over sharing the Kaveri waters began in 1807, when the Madras Presidency objected to the iirigation proposals by the Kingdom of Mysore. After initial discussions failed, the British authorities mediated a six-rule agreement known as the General Agreement of 1892. This agreement was revised in 1924 for a fifty-year term. Following its expiration in 1974, Karnataka sought a new allocation framework citing extended irrigation needs, while Tamil Nadu favored an extension of the agreement. Under article 262 of the Constitution of India, the central government is empowered to adjudicate interstate water disputes. Following a Supreme Court directive, the Union Government constituted the Cauvery Water Disputes Tribunal (CWDT) on 2 June 1990. On 25 June 1991, the ribunal issued an interim award directing Karnataka to release 205 tmc ft (5.80 km3) of water annually to Tamil Nadu, according to a prescribed monthly schedule. In the order passed on 25 June 1991, the CWDT directed Karnataka to release 205 tmcft of water per year to Tamil Nadu based on a specific schedule. Tamil Nadu was directed to release 6 tmc ft (0.17 km3) of water to Puducherry.
Implementation framework and CRA