River Cauvery

The Kaveri (also known as Cauvery, the anglicized name) is one of the major Indian rivers flowing through the states of Karnataka and Tamil Nadu. The Kaveri river rises at Talakaveri in the Brahmagiri range in the Western Ghats, Kodagu district of the state of Karnataka, at an elevation of 1,341 m above mean sea level and flows for about 800 km before its outfall into the Bay of Bengal. It reaches the sea in Poompuhar in Mayiladuthurai district. It is the third largest river after Godavari and Krishna in southern India, and the largest in the State of Tamil Nadu, which, on its course, bisects the state into north and south. In ancient Tamil literature, the river was also called Ponni (the golden maid, in reference to the fine silt it deposits).

The Kaveri is a sacred river to the people of South India and is worshipped as the Goddess Kaveriamma (Mother Cauvery). It is considered to be among the seven holy rivers of India. It is extensively used for agriculture in both Karnataka and Tamil Nadu.

The catchment area of the Kaveri basin is estimated to be with many tributaries including Harangi, Hemavati, Kabini, Bhavani, Lakshmana Tirtha, Noyyal and Arkavati. The river basin covers three states and a Union Territory as follows: Tamil Nadu, ; Karnataka, ; Kerala, , and Puducherry, . In Chamarajanagar district it forms the island of Shivanasamudra, on either side of which are the scenic Shivanasamudra Falls that descend about . The river is the source for an extensive irrigation system and for hydroelectric power. The river has supported irrigated agriculture for centuries and served as the lifeblood of the ancient kingdoms and modern cities of southern India. Access to the river's waters has pitted Indian states against each other for decades. It was profusely described in the Tamil Sangam literature and is held in great reverence in Hinduism. The Kaveri river delta is a thickly populated delta, one which is frequently affected by tropical cyclones formed in the Bay of Bengal.

Etymology

Dravidian

*The etymology of the river was derived from the Sankethi word for "river", ಕಾವೇರಿ காவிரி (kāviri), as this is the major river for the Sankethi people that live along its waters. The word is from the Dravidian/Tamil root words "ka" and "viri", "கா" and "விரி", which roughly translates to "branching into fields/forests", due to the river's multiple divergences in the delta region.
*Another likely Dravidian-origin of the word is from ''kāv'', meaning "forest", and ''ēri'' meaning "a large water body".

Sanskrit

*Another theory suggests that Kāvēri is a Sanskrit word, from ''Ka'' which means "of water" and ''Vēri'' can be translated as "whose body" in feminine. Thus ''Kāvēri'' is "she whose body is made of water".

Marudvṛdhā is another hypothesized name for this river, meaning "the beloved of the Maruts". However, Marudvrdhā is also identified with a river in Punjab.

Course

After the river leaves the Kodagu hills and flows onto the Deccan plateau, it forms two islands in Mandya district's Srirangapatna and Shivanasamudra. First comes the Srirangapatna, which forms the sangam, and then comes Shivanasamudra. At Shivanasamudra the river drops , forming the famous Shivanasamudra Falls known separately as ''Gagana Chukki'' and ''Bhara Chukki''. Asia's first hydroelectric plant (built in 1902) was on the left falls and supplied power to the city of Bangalore.

In its course through Karnataka, the channel is interrupted by 12 "anekattu" (dams) for the purpose of irrigation. From the Anaikattu at Madadkatte, an artificial channel is diverted at a distance of , irrigating an area of , and ultimately bringing its water supply to the town of Mandya.

3 km away from Srirangapatna, the Kaveri is the basis for the Ranganthittu Bird Sanctuary. Near Srirangapatna is also an aqueduct, the Bangara Doddi Nala, which was constructed in the 17th century by the Wodeyar maharaja of Mysore, Ranadhira Kantirava, in memory of his favourite consort. This aqueduct also served as a motorable bridge until 1964.The Kabini River tributary of Kaveri joins Kaveri at Tirumakudal Narasipura where triveni sangama takes place along with mythological river Spatika. The Moyar River is an east flowing river that originates in the Mudumalai, Bandipur, and Wayanad National Parks draining the Nilgiri Hills in Tamil Nadu and Karnataka and is one of the tributaries to the Kaveri River.

The river enters Tamil Nadu through Dharmapuri district leading to the flat plains where it meanders. It drops into the Hogenakkal Falls just before it arrives in the town of Hogenakkal in Tamil Nadu. The three minor tributaries, Palar, Chinnar and Thoppar enter into the Kaveri on her course, above Stanley Reservoir in Mettur, where the dam has been constructed. It then flows further through the length of Erode district where the river Bhavani, running through the breadth of the district, merges with it. The confluence of the rivers Kaveri, Bhavani and Akash Ganga (mythological) is at the exact place of Bhavani, Tamil Nadu Kooduthurai or Tiriveni Sangamam, Northern part of Erode City.

While passing through Erode, two more tributaries merge. Thirumani Mutharu joins it in a village called Kududurai in Namakkal District. Noyyal and Amaravathi join it in Karur district and reaches Mayanur Dam, about 20 km east of Karur city. Here the river becomes wide, with a sandy bed, and flows in an eastern direction to enter Tiruchirappalli district It splits into two at upper Anicut about west of Tiruchirappalli. The northern branch of the river is called the Kollidam at Ariyalur District while the southern branch retains the name Kaveri and then goes directly eastwards into Thanjavur District. These two rivers join again and form the Srirangam island that is a part of the city of Tiruchirapalli. The oldest functional dam Grand Anicut or Kallanai was present at this place. From Thanjavur, the river splits and goes to few places in the Kaveri delta .

Tributaries

* Harangi River
* Hemavati River
* Lakshmana Tirtha
* Amaravathi River
* Bhavani River
* Kabini River
* Noyyal River
* Arkavathi River
* Shimsha River
* Manimuttharu River
* Palar River (Kaveri basin)
* Moyar River

Irrigation

The primary uses of the Kaveri is providing water for irrigation, water for household consumption and the generation of electricity.

An estimate at the time of the first Five Year Plan puts the total flow of the Kaveri at , of which 60% was used for irrigation.

The Torekadanahalli pumpstation sends per day of water from the Kaveri to Bangalore.

The hydroelectric plant built on the left of Sivanasamudra Falls on the Kaveri in 1902 was the first hydroelectric plant in Asia.

The Krishna Raja Sagara Dam has a capacity of 49 tmc ft. and the Mettur Dam which creates Stanley Reservoir has a capacity of 93.4 tmc ft. (thousand million cubic ft)

In August 2003, inflow into reservoirs in Karnataka was at a 29-year low, with a 58% shortfall. Water stored in Krishna Raja Sagara amounted to only 4.6 tmc ft.

In February 2020, Tamil Nadu assembly passed bill to declare Cauvery Delta as Protected Agricultural Zone, includes Thanjavur, Thirvarur, Nagapattinam and five blocks in Cuddalore and Pudukottai. The bill fails to include Tiruchirappalli, Ariyalur and Karur which are geographically included in the Cauvery Delta.

Water sharing

Per the order of the Indian Supreme Court on 16 February 2018, Karnataka will get 284.75 tmc ft, Tamil Nadu will get 404.25 tmc ft, Kerala will get 30 tmc ft and Puducherry will get 7 tmc ft. 10 tmc ft will be reserved for Environmental Protection and 4 tmc ft will be reserved for Inevitable Wastage into the Sea.

Cauvery Water Management Authority (CWMA) and Cauvery Water Regulation Committee (CWRC) 2018

Acting on the Supreme Court's direction, the Centre constituted a Cauvery Water Management Authority (CWMA) on 1 June 2018 to address the dispute over sharing of river water among Tamil Nadu, Karnataka, Kerala and Puducherry. The central government failed to adhere with the top court's deadline of within six weeks of deliverance of judgement.

On 16 February 2018, the apex court had directed the government to form the CWMA within six weeks in a verdict that marginally increased Karnataka's share of Cauvery water, reduced the allocation for Tamil Nadu and sought to settle the protracted water dispute between the two states.

On 22 June 2018, despite opposition from Karnataka, the Central government constituted the Cauvery Water Regulation Committee (CWRC) as per the provisions in the Kaveri Management Scheme laid down by the Supreme Court.

Central Water Commission chairman S. Masood Hussain will head the CWMA and chief engineer of the Central Water Commission Navin Kumar will be the first chairman of the CWRC. While the CWMA is an umbrella body, the CWRC will monitor water management on a day-to-day basis, including the water level and inflow and outflow of reservoirs in all the basin states.

Kaveri Crater

Kaveri Crater is an area identified by scientists in India which appears to have been created by an asteroid impact that occurred around 800 to 550 million years ago. The area lying between Nilgiris and Kodaikanal is in the southern peninsular India. A study indicated that the Kaveri crater has a diameter of 120 kilometers. Because of the size of the crater, Kaveri crater can only be visualized through satellite images. The crater is the fourth largest crater in the world.

The region to the east of Palghat gap is of low elevation and nearly circular in shape. It forms a part of the Kaveri river basin. The predominantly gneissic terrain is surrounded by the charnockitic hill ranges, prominent among which are Nilgiris and Biligiriranga Hills to the north; and Anaimalai and Kodaikanal to the south. The charnockite massifs have a steep slope facing the circular feature and a gentler slope in the opposite direction. Fractures, faults and shear zones are noticed in many parts. The Bouguer anomaly in the gneissic terrain is elliptical in shape and positive, relative to the surrounding elevated region. The magnetic contours are also elliptical and the magnetic basement is deeper by about one kilometer compared with regions in the periphery. The shallow seismic velocity picture from Chennimalai to Palani indicates a graben structure. The velocity structure also depicts a 4-5 kilometer Moho up-warp near Chennimalai. Junction between the gneissic and charnockitic terrain and even beyond is marked by the presence of pseudotachylites and breccia. Field and petrographic studies indicate presence of suevite, planar deformation features (PDF), planar fractures, diaplectic glass of quartz and plagioclase and spherical inclusion in suevite. These evidences taken together point to an extraterrestrial impact that created a crater of approximately 120 kilometer in diameter. Several lines of indirect evidences point to Neoproterozoic age for the impact.

See also

* List of rivers of India
* Kaveri Pushkaram

References

External links

Cauvery
Presentation on the Cavery River

Kaveri Pushkaralu

Kaveri Pushkaram 2017

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Rivers of Tamil Nadu
Rivers of Karnataka
Ancient Indian rivers
Sacred rivers
Coromandel Coast
Rivers of India
Rivers in Buddhism