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{{Short description|River in southern India}} | |||
{{cleanup-tone}}{{unreferenced}} | |||
{{About|the river|other uses}} | |||
{{Use Indian English|date=July 2019}} | |||
{{Use dmy dates|date=January 2018}} | |||
{{Infobox river | |||
| name = Kaveri | |||
| name_other = Cauvery | |||
<!---------------------- IMAGE & MAP --> | |||
| image = {{Photomontage | |||
| photo1a = Thalakkaveri_Temple,_Karnataka.jpg | |||
| photo1b = Kaveri_View_Rail_Bridge_Srirangapatna_Jul22_A7C_02120.jpg | |||
| photo2a = Barahachukki.jpg | |||
| photo2b = Hogenakkal_Falls_Close.jpg | |||
| photo3a = Bhavani-Kaveri-Sangamam.JPG | |||
| photo3b = Grand Anaicut.jpg | |||
| foot_montage = '''Clockwise from top left''': ]; Kaveri at ]; ]; ]; Confluence with ]; and ] | |||
| size = 250 | |||
| position = center | |||
}} | |||
| map_size = 250px | |||
| map = Cauvery River Basin.png | |||
| map_caption = Kaveri River basin | |||
| pushpin_map = | |||
| pushpin_map_size = | |||
| pushpin_map_caption = | |||
<!---------------------- LOCATION --> | |||
| subdivision_type1 = Country | |||
| subdivision_name1 = India | |||
| subdivision_type2 = Region | |||
| subdivision_name2 = ] | |||
| subdivision_type3 = States | |||
| subdivision_name3 = ], ], ], ] | |||
<!---------------------- PHYSICAL CHARACTERISTICS --> | |||
| length = {{cvt|800|km}}<ref name="Data">{{cite report|url=http://www.cwc.nic.in/main/downloads/IHD2015_final.pdf|title=Integrated Hydrological Data Book|publisher=]|page=92|access-date=13 November 2017|archive-url=https://web.archive.org/web/20160402104009/http://www.cwc.nic.in/main/downloads/IHD2015_final.pdf|archive-date=2 April 2016|url-status=dead|df=dmy-all}}</ref> | |||
| width_min = | |||
| width_avg = | |||
| width_max = | |||
| depth_min = | |||
| depth_avg = | |||
| depth_max = | |||
| discharge1_location = ] (58.5 km upstream of mouth) | |||
| discharge1_min = {{cvt|144|m3/s}}<ref name="Discharge1">{{cite web|url=https://floodobservatory.colorado.edu/SiteDisplays/2043.htm|title=River Discharge and Reservoir Storage Changes - Area 2043|work=Flood observatory, ]|access-date=1 June 2024}}</ref> | |||
| discharge1_avg = {{cvt|919|m3/s}} (1998-2024)<ref name="Discharge1"/> | |||
| discharge1_max = {{cvt|4,075|m3/s}}<ref name="Discharge1"/> | |||
| discharge2_location = ] (140 km upstream of mouth) | |||
| discharge2_min = {{cvt|78|m3/s}}<ref name="Discharge2">{{cite web|url=https://floodobservatory.colorado.edu/SiteDisplays/2042.htm|title=River Discharge and Reservoir Storage Changes - Area 2042|work=Flood observatory, ]|access-date=1 June 2024}}</ref> | |||
| discharge2_avg = {{cvt|400.716|m3/s}} (1976-1979)<ref name="Discharge3">{{cite web|title=Gauging Station - Data Summary|work=RivDis|url=http://daac.ornl.gov/rivdis/STATIONS/TEXT/INDIA/1263/SUMMARY.HTML|access-date=1 October 2013|url-status=dead| archive-url = https://web.archive.org/web/20131004215927/http://daac.ornl.gov/rivdis/STATIONS/TEXT/INDIA/1263/SUMMARY.HTML|archive-date = 4 October 2013| df=dmy-all}}</ref> <br/> {{cvt|1,131|m3/s}} (1998-2024)<ref name="Discharge2"/> | |||
| discharge2_max = {{cvt|4,916|m3/s}}<ref name="Discharge2"/> | |||
<!---------------------- BASIN FEATURES --> | |||
| source1 = ] | |||
| source1_location = ], ], Karnataka | |||
| source1_coordinates = {{coord|12|23|N|75|29|E|display=inline}} | |||
| source1_elevation = {{cvt|1,341|m}} | |||
| mouth = ] | |||
| mouth_location = ], ], Tamil Nadu | |||
| mouth_coordinates = | |||
| mouth_elevation = {{cvt|0|m}} | |||
| progression = | |||
| river_system = | |||
| basin_size = {{cvt|81,155|km2}}<ref name="Riparian">{{cite web|url=https://jalshakti-dowr.gov.in/cauvery-water-dispute/|title=Cauvery Water|work=], ]|access-date=1 June 2024}}</ref> | |||
| tributaries_left = ], ], ], ], ], ] | |||
| tributaries_right = ], ], ], ], ], ] | |||
| custom_label = | |||
| custom_data = | |||
| extra = | |||
}} | |||
The '''Kaveri''' (also known as '''Cauvery''') is a ] flowing across ]. It is the third largest river in the region after ] and ]. | |||
The catchment area of the Kaveri basin is estimated to be {{cvt|81155|km2}} and encompasses the states of ], ], ], and the union territory of ]. | |||
The river rises at ] in the ] range in the ]. The source is located at an elevation of {{cvt|1,341|m}} in the ] of Karnataka. The river flows for about {{cvt|320|km}} through the ] in Karnataka before entering Tamil Nadu. It flows further eastward in Tamil Nadu for {{cvt|416|km}} before flowing into the ] near ] in ] of Tamil Nadu. The river flows for a total length of about {{cvt|800|km}}. The major tributaries include ], ], ], ], ], ], and ]. | |||
] | |||
There are a number of dams on the river which form part of an extensive ] and are used for the generation of ]. The river has supported agriculture for centuries and has served as the lifeline of several kingdoms in the past. Access to the river's waters has been a ] among the states of Karnataka and Tamil Nadu for decades. The Kaveri basin is a densely populated region, with several towns and cities located on its banks. | |||
The '''Kaveri River''' (]: ಕಾವೇರಿ, {{lang-ta|காவிரி}}, also spelled ''Cauvery'' or ''Kaveri'' in English) is one of the great rivers of ] and is considered sacred by the ]. The river originates at ] in the ] in the state of ], flows generally south and east through ] and ] and across the southern ] through the southeastern lowlands, emptying into the ] through two principal mouths. | |||
The river is considered as sacred by the people of Southern India and is considered to be among the seven holy rivers of India. The river is often personified and worshiped as the goddess Kaveri. The river is mentioned in various Hindu religious texts including the '']'' and the '']''. In ancient ], the river is referenced to as ''Ponni'' meaning "the golden one". | |||
The Kaveri River basin is estimated to be 27,700 square miles with many tributaries including the ], the ], the ], the ], ], ], ], ], the ], the ] and the ]. | |||
== Etymology == | |||
The river has supported irrigated agriculture for centuries and served as the lifeblood of the ancient kingdoms and modern cities of ]. | |||
Kaveri is mentioned in ] as a holy river in various Hindu religious texts including the '']'' and the '']''.<ref name="Wisdom">{{cite web|url=https://www.wisdomlib.org/definition/kaveri|title=Kaveri|work=Wisdom library|access-date=1 June 2024}}</ref> The name itself might have had different etymologies. As per '']'', the river arose after ] took a form of a crow and toppled sage ]'s ]. The river then took its name from the ] words ''kā'' meaning "crow" and ''viri'' meaning "spread" literally translating to "spread by a crow". It might also mean a river with wide spread banks as ''viri'' can also be translated as wide spread.<ref name="Wisdom"/><ref>{{cite web|url=https://tamil.samayam.com/religion/temples/story-of-river-kaveri-how-lord-ganesha-and-maharshi-agasthiyar-started-river-cauvery/articleshow/70820021.cms|title=River Kaveri Story|date=9 September 2021|access-date=1 June 2024|work=Samayam|lang=ta}}</ref><ref name="Pao">{{cite web|url=https://e-pao.net/epSubPageExtractor.asp?src=travel.Manipur_Travel_Log.Cauvery_flows_thanks_to_a_crow_By_S_Balakrishnan|title=Cauvery flows, thanks to a crow!|date=4 January 2024|access-date=1 June 2024|work=E-pao}}</ref> The etymology of the river might have also been derived from ''kāviri'', the ] word for "river" from the language spoken by the ], who live along its waters.<ref>{{cite web|url=https://www.outlookindia.com/travel/how-the-rivers-of-india-descended-from-the-heavens-kaveri-news-185689|title=How the Rivers of India Descended From the Heavens: Kaveri|date=5 November 2022|access-date=1 June 2024|work=]}}</ref> Cauvery is the ] version of the original name.<ref name="Pao"/> | |||
== Mythic origin == | |||
The Kaveri may be called by devout ]s as Dakshina Ganga, or the ] of the south, and the whole of its course is holy ground. According to the legend there was once born upon earth a girl named Vishnumaya or Lopamudra, the daughter of ], but her divine father permitted her to be regarded as the child of a mortal called Kavera-muni. In order to obtain beatitude for her adoptive father, she resolved to become a river whose waters should purify all sin. Hence it is said that even the holy Ganges resorts to going underground once in the year to the source of the Kaveri, to purge herself from the pollution contracted from the crowd of sinners who have bathed in her waters. | |||
The river is also known by other names. In ancient ], the river was called ''Ponni'' meaning "the golden one" in reference to the fine silt it deposits.<ref>{{cite web|url=https://indianexpress.com/article/india/india-others/daughter-of-ponni/|title=Daughter of Ponni|date=27 April 2014|work=]|access-date=27 April 2014}}</ref><ref>{{cite web|url=https://www.newslaundry.com/2020/02/08/cauvery-chronicles-ii-ponnis-perish|title=Cauvery Chronicles II: Ponni's Perish|work=Newslaundry|date=8 February 2020|access-date=8 February 2020}}</ref><ref>{{cite web|url=http://www.millenniumpost.in/opinion/the-death-of-a-river-357460|title=The death of a river|date=11 June 2019|work=Millennium Post|access-date=11 June 2019}}</ref> It is known as ''Daksina gaṅgā'' meaning the "] of the South" indicating its geographical location and its significance.<ref name="Brit">{{cite encyclopedia|title=Kaveri River|url=https://www.britannica.com/place/Kaveri-River|encyclopedia=]|access-date=1 June 2024}}</ref> It is also mentioned as ''Ardha gaṅgā'' meaning ''Half Ganga'' in Mahabharata and other literature, due to its purported mythology of having arisen from the Ganges.<ref name="Wisdom"/> Marudvṛdhā is another hypothesised name for this river, meaning "the beloved of the ]" in Sanskrit.<ref>{{cite web|title=Marudvṛdhā|url=https://www.sanskrit-lexicon.uni-koeln.de/scans/MWScan/2020/web/index.php|access-date=18 July 2022|work=Sanskrit Lexicon}}</ref> | |||
==River course== | |||
After the river leaves the Kodagu hills, to flow on to the Deccan plateau, it has three islands, ] and ] in Karnataka and ] in Tamil Nadu. At Sivasamudra island the river drops 320 ft (98 m), forming famous falls known as Gagan chukki and Bara Chukki. India's first ] plant (built in 1902) was on the left falls and supplied power to the city of ]. Bangalore when electrified in 1906, was the first city in Asia to be electrified and to have electric street lights. | |||
== |
== Course == | ||
The river arises at ] in ] of ].<ref name="Springer">{{cite book |last1=Jain |first1=Sharad K. |url=https://books.google.com/books?id=ZKs1gBhJSWIC&dq=kaveri+river+course&pg=PA702 |title=Hydrology and Water Resources of India |last2=Agarwal |first2=Pushpendra K. |last3=Singh |first3=Vijay P. |publisher=] |year=2007 |pages=702–711|isbn=9781402051807 }}</ref> The source of the river is located at an altitude of {{cvt|1,341|m}} in the ] of the ].<ref name="Data"/> Its follows a rough upper course consisting of rocky beds and high banks. Once it leaves the Kodagu hills, it flows eastwards and forms a series of rapids and falls. It flows through a narrow gorge onto the ] and drops about {{cvt|18-24|m}} at ].<ref name="Brit"/> The river forms the island of ] and widens to {{cvt|900-1200|ft}} before flowing south-east.<ref name="Brit"/><ref name="Springer"/> At ], the river drops {{cvt|91|m}} and forms the ], one of the largest waterfalls in the country.<ref name="Data"/><ref name="Springer"/> After forming the island of Shivanasamudra, the river converges and passes through the ] gorge.<ref name="Data"/><ref name="Singh">{{cite book|last=Singh|first=Dhruv Sen|title=The Indian rivers : scientific and socio-economic aspects|publisher=]|year=2018|location=Singapore|pages=354–356}}</ref> After flowing for {{cvt|320|km}} in Karnataka, the river flows for about {{cvt|64|km}} along the Karnataka-] border.<ref name="Data"/> | |||
In its course through Karnataka the channel is interrupted by twelve anicuts or dams for the purpose of irrigation. From the anicut at Madadkatte, an artificial channel is led to a distance of 72 miles, irrigating an area of 10,000 acres (40 km²), and ultimately bringing a water-supply into the town of Mysore. Near Srirangapatna, there is an ancient aqueduct, the Bangara Doddi Nala, which was constructed by the ] ruler Ranadhira Kantirava in memory of his favorite consort. It is said to be the only aqueduct where the water from the very same river, dammed upstream, is carried by the aqueduct over the very same river few miles downstream {{citation needed}}. This aqueduct also served as a motorable bridge till ]. There are many ancient and modern canals from the river for irrigational purposes. It also serves as the main drinking water source for many towns and villages. The cities of Bangalore and Mysore depend almost entirely on Kaveri for their drinking water supply. | |||
The river enters Tamil Nadu and forms the ].<ref name="Springer"/> After the falls, the river flows southwards towards ] and joins its main right bank tributary ] at ].<ref name="Data"/><ref name="Singh"/> The river flows eastwards through ] and ], and widens further before entering the ]. It splits into two branches with the northern part called as ] and the southern part of the river retaining the name Kaveri.<ref name="Data"/> After flowing for {{cvt|16|km}}, the two branches converge around the ] island.<ref name="Data"/><ref name="Singh"/> The river further branches off into 36 different channels before emptying into the ] near ] in ].<ref>{{cite book |last1=Ramkumar |first1=Mu |url=https://books.google.com/books?id=9Yq9BgAAQBAJ&dq=kaveri+delta&pg=PA286 |title=Environmental Management of River Basin Ecosystems |last2=Kumaraswamy |first2=K. |last3=Mohanraj |first3=R. |publisher=] |year=2015 |pages=286}}</ref> The river traverses for about {{cvt|416|km}} in Tamil Nadu for a total length of about {{cvt|800|km}}.<ref name="Data"/> | |||
== Kaveri in Tamil Nadu == | |||
After entering Tamil Nadu, the Kaveri forms the boundary between the ] and the ] district. The ] joins the Kaveri at the town of ], where the ], an important pilgrimage spot in southern India, was built at the confluence of the two rivers. The ] joins the Kaveri at a place called Tirumukkudalur near ]. | |||
=== Tributaries === | |||
Sweeping past the historic rock of ], it breaks at the island of ] into two channels, which enclose between them the delta of ] (Tanjore), the "rice bowl" of ] and garden of south india. The northern channel is called the ] (Coleroon). The other channel keeps the name of Kaveri and empties into the ] at ], a few hundred miles south of ] in ]. On the seaward face of its delta are the seaports of ] and ]. | |||
The Kaveri River has 21 major tributaries.<ref name="Data"/> The largest tributary ], and ] join the river at ].<ref name="Data"/><ref name="Brit"/> ] is another major contributor to the flow of Kaveri and joins the river in Karnataka. It meets with its second largest tributary ] at ] in ] and two other tributaries ], and ] join further down the stream in Tamil Nadu.<ref name="Data"/> Other tributaries of Kaveri include ], ], ], and ].<ref name="Data"/><ref name="Singh"/> | |||
=== Discharge === | |||
The most ancient surviving irrigation work is the ] or '']'', a massive dam of unhewn stone, 328 meters (1080 feet) long and 20 meters (60 feet) wide, spanning the stream of the Kaveri proper. The area irrigated by the ancient tank system was 69,000 acres{{fact}} (280 km²), which by the early ] increased to about 1,000,000 acres{{fact}} (4,000 km²) and later drastically reduced after the construction of other dams upstream{{fact}}. | |||
Source:<ref name="Discharge1"/><ref name="Discharge2"/> | |||
{| class="wikitable mw-collapsible mw-collapsed" style="text-align:center;" | |||
|+Discharge | |||
! rowspan="3" |Year | |||
! rowspan="28" | | |||
! colspan="3" |] | |||
! rowspan="28" | | |||
! colspan="3" |] | |||
|- | |||
! colspan="3" |<nowiki> </nowiki>(m<sup>3</sup>/s) | |||
! colspan="3" |(m<sup>3</sup>/s) | |||
|- | |||
!Min | |||
!Mean | |||
!Max | |||
!Min | |||
!Mean | |||
!Max | |||
|- | |||
|1998 | |||
|170 | |||
|1,099 | |||
|3,454 | |||
|161 | |||
|885 | |||
|2,540 | |||
|- | |||
|1999 | |||
|289 | |||
|1,131 | |||
|3,778 | |||
|285 | |||
|864 | |||
|2,845 | |||
|- | |||
|2000 | |||
|343 | |||
|1,287 | |||
|4,903 | |||
|233 | |||
|1,011 | |||
|3,335 | |||
|- | |||
|2001 | |||
|258 | |||
|1,080 | |||
|3,348 | |||
|309 | |||
|948 | |||
|3,115 | |||
|- | |||
|2002 | |||
|139 | |||
|772 | |||
|2,392 | |||
|144 | |||
|867 | |||
|2,423 | |||
|- | |||
|2003 | |||
|78 | |||
|667 | |||
|2,297 | |||
|216 | |||
|646 | |||
|2,100 | |||
|- | |||
|2004 | |||
|103 | |||
|895 | |||
|3,303 | |||
|217 | |||
|839 | |||
|3,160 | |||
|- | |||
|2005 | |||
|179 | |||
|1,012 | |||
|3,354 | |||
|240 | |||
|991 | |||
|3,873 | |||
|- | |||
|2006 | |||
|268 | |||
|1,072 | |||
|2,495 | |||
|473 | |||
|1,091 | |||
|3,187 | |||
|- | |||
|2007 | |||
|118 | |||
|993 | |||
|3,308 | |||
|324 | |||
|1,126 | |||
|4,075 | |||
|- | |||
|2008 | |||
|132 | |||
|1,094 | |||
|3,677 | |||
|398 | |||
|1,103 | |||
|3,167 | |||
|- | |||
|2009 | |||
|227 | |||
|1,040 | |||
|3,238 | |||
|290 | |||
|965 | |||
|3,301 | |||
|- | |||
|2010 | |||
|373 | |||
|1,080 | |||
|3,141 | |||
|411 | |||
|1,022 | |||
|3,626 | |||
|- | |||
|2011 | |||
|171 | |||
|1,163 | |||
|3,815 | |||
|296 | |||
|928 | |||
|3,014 | |||
|- | |||
|2012 | |||
|190 | |||
|874 | |||
|3,342 | |||
|177 | |||
|711 | |||
|2,149 | |||
|- | |||
|2013 | |||
|82 | |||
|1,043 | |||
|3,281 | |||
|229 | |||
|856 | |||
|3,127 | |||
|- | |||
|2014 | |||
|279 | |||
|1,148 | |||
|3,663 | |||
|409 | |||
|980 | |||
|2,533 | |||
|- | |||
|2015 | |||
|559 | |||
|1,422 | |||
|3,816 | |||
|407 | |||
|913 | |||
|2,177 | |||
|- | |||
|2016 | |||
|490 | |||
|1,129 | |||
|2,890 | |||
|276 | |||
|728 | |||
|1,733 | |||
|- | |||
|2017 | |||
|216 | |||
|931 | |||
|3,586 | |||
|154 | |||
|671 | |||
|1,832 | |||
|- | |||
|2018 | |||
|341 | |||
|1,571 | |||
|4,439 | |||
|266 | |||
|934 | |||
|3,427 | |||
|- | |||
|2019 | |||
|331 | |||
|1,473 | |||
|4,559 | |||
|173 | |||
|966 | |||
|3,070 | |||
|- | |||
|2020 | |||
|591 | |||
|1,590 | |||
|4,373 | |||
|209 | |||
|983 | |||
|2,944 | |||
|- | |||
|2021 | |||
|478 | |||
|1,502 | |||
|3,935 | |||
|257 | |||
|988 | |||
|3,136 | |||
|- | |||
|2022 | |||
|548 | |||
|1,713 | |||
|4,916 | |||
|407 | |||
|1,172 | |||
|3,385 | |||
|- | |||
!Overall | |||
! | |||
!78 | |||
!1,151 | |||
!4,916 | |||
! | |||
!144 | |||
!928 | |||
!4,075 | |||
|} | |||
== Geology and ecology == | |||
The chief ] work is the anicut across the Kollidam 2250 ft. long, constructed by Sir ] between ] and ]. The ] is the most ancient surviving irrigation work in the ] ].The dam is still in excellent repair, and supplied a model to later engineers. | |||
] | |||
The Kaveri basin was formed in the ] to ] period during ] breakup and opening of the ].<ref>{{cite journal |last1=Nagendra |first1=R. |last2=Nallapa Reddy |first2=A. |date=2017 |title=Major geologic events of the Cauvery Basin, India and their correlation with global signatures – A review |journal=Journal of Palaeogeography |volume=6 |issue=1 |pages=69–83 |doi=10.1016/j.jop.2016.09.002 |doi-access=free }}</ref> Most of the basin is made up of ] rocks and the two major rock types that are found are ] and ] rocks.<ref name="Singh"/> Closepet granite is found in the upper parts of the Kaveri basin and ] rocks are only found in the central part.<ref name="Springer"/> A 2017 paper proposed that an ] was present in the vicinity of the Kaveri river.<ref>{{cite journal |last1=Subrahmanya |first1=K. R. |last2=Prakash Narasimha |first2=K. N. |date=October 2017 |title=Kaveri crater – An impact structure in the Precambrian terrain of southern India |url=http://link.springer.com/10.1007/s12594-017-0733-5 |journal=Journal of the Geological Society of India|volume=90 |issue=4 |pages=387–395 |doi=10.1007/s12594-017-0733-5 |s2cid=134717819 |issn=0016-7622}}</ref> The run-off from the river does not drain off quickly because of the shape of the river basin, which limits the occurrence of floods. It is a ] fed mostly by ]s. Four distinct seasons occur in the basin with hot and cold seasons sandwiching the monsoon seasons. The river basin is fed by South-West monsoon in Karnataka, and North-East monsoon in Tamil Nadu.<ref name="Data"/> | |||
== Water sharing== | |||
Kaveri water sharing has been a major issue of contention between the states of Karnataka, Tamil Nadu, Kerala and the union territory of Pondicherry. A central government agency has been formed to look into this issue. | |||
The Kaveri basin is made up of two sub-zones, forest and agro-ecosystem.<ref name="Environ"/> The forest vegetation consists of a mix of ], ], and ].<ref name="Compendium"/> As per a study, about {{cvt|12,850|km2}} of natural vegetation was lost in the river basin between 1965 to 2016.<ref>{{cite news|url=https://www.thehindu.com/sci-tech/energy-and-environment/natural-vegetation-on-nearly-12850-sq-km-in-the-cauvery-basin-has-been-lost-says-a-research-paper/article67624533.ece|title=Natural vegetation on nearly 12,850 sq. km in the Cauvery basin has been lost, says a research paper|newspaper=]|date=11 December 2023|access-date=1 June 2024}}</ref> The basin has a variety of flora with major species including '']'', '']'', '']'', '']'', '']'', '']'', '']'', and '']''.<ref name="Environ">{{cite journal |last1=Sunil |first1=C. |last2=Somashekar |first2=R. K. |last3=Nagaraja |first3=B. C. |date=2010-11-01 |title=Riparian vegetation assessment of Cauvery River Basin of South India |url=https://doi.org/10.1007/s10661-009-1256-3 |journal=Environmental Monitoring and Assessment |volume=170 |issue=1 |pages=548 |doi=10.1007/s10661-009-1256-3|pmid=20024615 |s2cid=19865294 }}</ref> | |||
According to a study conducted by the central government in 1972, the utilisation of water from Cauvery in Tamil Nadu was 489 tmc against Karnataka's 177 tmc. Now Karnataka wants to utilise 465 tmc, against its present usage of 312.32 tmc. It is against this background that Tamil Nadu went to the Supreme Court. | |||
There are many ] spread across the river basin including significant ] and ] habitats. The basin provides habitat to a range of animal species such as ], ], ], ], ], ], ], and various species of deer, wild boar and reptiles.<ref name="Compendium">{{cite report|url=https://tourism.gov.in/sites/default/files/2023-04/9%20Compendium%20Book_2021_Low%20%281%29%20%282%29.pdf|title=National Parks and Wildlife Sanctuaries in India|work=], ]|date=November 2021|access-date=1 June 2024}}</ref> The river also hosts a variety of avifauna including the ] (''Mycteria leucocephala''), ] (''Pelecanus philippensis''), and ] (''Threskiornis melanocephalus''). It is also home to the ] (''Crocodylus palustris''), ] ''(Lutrogale perspicillata),'' and ] ''(Tor remadevii).''<ref>{{cite web |title=Ranganathittu Bird Sanctuary|work=Ramsar Sites Information Service |url=https://rsis.ramsar.org/ris/2473 |access-date=18 February 2023}}</ref> | |||
The Cauvery Tribunal, in its interim award of June 1991, ordered that Karnataka should release 205 tmc of water to Tamil Nadu during one water year, that is from May to June. It also stipulated a weekly quantum of flow. Karnataka has scrupulously followed the interim order and released '''much more''' than 205 TMC of water every year except in the year '95-'96 when the shortfall was merely about 10%(, ) | |||
== |
== Riparian zone == | ||
] formed by ], the largest dams on the river.]] | |||
* ] | |||
* ] | |||
* ] | |||
* ] | |||
* ] (meaning "smoking rock"): The spray of the river hitting the rocks is so fine that it appears like smoke | |||
* ] (Goat's Leap) | |||
* ] (Trichy) | |||
* ] | |||
* ] | |||
* ] | |||
The total watershed of the basin is {{cvt|81,155|km2}} and the ] of the river consists of {{cvt|43,856|km2}} in Tamil Nadu, {{cvt|34,273|km2}} in Karnataka, {{cvt|2,866|km2}} in ], and {{cvt|160|km2}} in the union territory of ].<ref name="Riparian"/><ref name="Data"/> Over half of the Kaveri basin is arable and the most cultivated crops are ] and ].<ref name="Environ"/> An estimate at the time of the first ] put the total flow of the river at {{convert|12000000|acre.ft|km3|order=flip}}, of which 60% was used for irrigation.<ref>{{cite web | url=http://planningcommission.nic.in/plans/planrel/fiveyr/1st/1planch26.html | title=Chapter 26: Irrigation and power | work=1st Five Year Plan | publisher=] | access-date=1 July 2019 | archive-url=https://web.archive.org/web/20190328061837/http://www.planningcommission.nic.in/plans/planrel/fiveyr/1st/1planch26.html | archive-date=28 March 2019 | url-status=dead }}</ref> The river is also used for ] and ] generation.<ref name="Brit"/><ref>{{cite web |url=http://www.tce.co.in/infra/watersupply/bangalore.pdf#search=%22halli%20pipeline%20Bangalore%22 |title=Archived copy |work=TCE|access-date=13 January 2022 |archive-url=https://web.archive.org/web/20070320070821/http://www.tce.co.in/infra/watersupply/bangalore.pdf#search=%22halli%20pipeline%20Bangalore%22 |archive-date=20 March 2007 |url-status=dead}}</ref> | |||
== Religious significance== | |||
] is a ] site set amidst Bramahagiri Hills in ]. Thousands of piligrims flock to the three temple at the source of the river especially on the specified day known as Tula sankramana when the river water has been said to gush out like a fountain at a predetermined time. | |||
The ] was constructed by a ] King in 2nd century CE.<ref name="Data"/> The hydroelectric plant built on the Sivanasamudra Falls in 1902 was the first hydroelectric plant in Asia.<ref>{{cite web|url=http://www.world-waterfalls.com/waterfall.php?num=149|title=World Waterfall Database|access-date=9 November 2006|archive-url=https://web.archive.org/web/20061114204057/http://www.world-waterfalls.com/waterfall.php?num=149|archive-date=14 November 2006|url-status=dead}}</ref> | |||
The three major river islands have a strong ] heritage, with sculptures of ] in a reclining posture on the legendary seven-headed Serpent as the celestial bed ''(Sheshashayana)''. These three temples are known as 'Adi Ranga', 'Madya Ranga' and 'Anthya Ranga'. | |||
The ] in Tamil Nadu was constructed in 1934 and the ] formed by the dam has a capacity of 93.4 ].<ref name="Brit"/><ref name="Res">{{cite web|url=http://tnagriculture.in/ARS/home/reservoir|title=Reservoir levels|work=]|access-date=1 June 2024}}</ref> ] in Karnataka is the second largest dam on the river and has a capacity of 49.5 ].<ref name="Res"/><ref>{{cite news| url=http://www.hindu.com/2006/03/26/stories/2006032614180300.htm | archive-url=https://web.archive.org/web/20061029044318/http://www.hindu.com/2006/03/26/stories/2006032614180300.htm | url-status=dead | archive-date=29 October 2006 | newspaper=] | title=Corporation urged to chalk out water policy for Mysore city | date=26 March 2006}}</ref> ] (32.8 tmc ft) on the ] in Tamil Nadu, Hemavathy Dam (37.1 tmc ft) on the ], ] (18.5 tmc ft) on the ], and ] (9.5 tmc ft) on the Harangi River in Karnataka are major dams on the tributaries of Kaveri.<ref name="Riparian"/><ref name="Res"/> | |||
=== Water dispute === | |||
The ] is located here. | |||
] | |||
{{further|Kaveri River water dispute}} | |||
The dispute over the sharing of Kaveri waters began in 1807 when the ] objected to the plans of the ] to develop irrigation projects. After initial discussions failed, the ] intervened and a six rule agreement called the ''General Agreement of 1892'' was signed.<ref>{{cite journal |last1=Rani |first1=Midatala |last2=Rani |first2=Middatala |date=2002 |title=Historical Background Of The Cauvery Water Dispute |url=https://www.jstor.org/stable/44158173 |journal=Proceedings of the Indian History Congress |volume=63 |pages=1033–1042 |jstor=44158173 }}</ref> After ], article 262 of the ] provided powers to the ] to adjudicate on inter-state disputes on water sharing.<ref>{{cite web|url=https://indiankanoon.org/doc/1558821/|title=Article 262 of Indian Consitution|work=Indiakanoon|access-date=1 June 2024}}</ref> The Government of India constituted the Cauvery Water Disputes Tribunal (CWDT) on 2 June 1990 to adjudicate the water dispute between the riparian states and territories in the river basin. In an order passed in June 1991, the CWDT directed Karnataka to release 205 tmc ft of water per year to Tamil Nadu based on a specific schedule. The water was to be released in four equal installments in a particular month and any shortfall would need to be covered in the subsequent week. Tamil Nadu was directed to provide 6 tmc ft of water to Puducherry.<ref name="Riparian"/> | |||
=References= | |||
<div class="references-small"> | |||
<references /> | |||
</div> | |||
In July 1991, the ] asked the ] to rule on the validity and legality of the tribunal under the Constitution. In November 1991, the Supreme Court opined that the order needs to be published by the central government in the Official Gazette, which was done on 1 December 1991.<ref name="Riparian"/> In May 1992, the ] filed a case in the Supreme Court to direct the Indian Government to pass necessary orders to ensure the implementation of the provisions of the tribunal order. In April 1997, the ] reverted that the central government has prepared a scheme under the Inter-State Water Disputes Act, 1956 for the implementation of the tribunal award and the Cauvery Water Authority (CRA) and Cauvery Monitoring Committee (CMC) were formed subsequently as a part of the Cauvery Water (Implementation of Interim Orders of 1991 and all subsequent Tribunal Orders) Scheme, 1998. The CRA is headed by the ] and consists of the Chief Ministers of the riparian states as its consituent members.<ref name="Riparian"/> | |||
==External link== | |||
* | |||
On 16 February 2018, the Supreme Court ruled that 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 of water from the river. An additional 10 tmc ft was reserved for environmental protection and 4 tmc ft was reserved for wastage into the sea.<ref>{{cite web |url=http://sci.gov.in/supremecourt/2007/11993/11993_2007_Judgement_16-Feb-2018.pdf |title=Archived copy |access-date=24 July 2018 |archive-url=https://web.archive.org/web/20180417132747/http://sci.gov.in/supremecourt/2007/11993/11993_2007_Judgement_16-Feb-2018.pdf |archive-date=17 April 2018 |url-status=dead }}</ref> The court directed the government to form a Cauvery Water Management Authority (CWMA) within six weeks and acting on the Supreme Court's direction, the central government constituted the CMWA in June 2018.<ref>{{cite news|url=https://www.thehindu.com/news/national/supreme-court-reduces-allocation-of-cauvery-water-to-tamil-nadu/article22771422.ece|title=Supreme Court curtails Tamil Nadu's share of Cauvery water|last=Rajagopal|first=Krishnadas|date=16 February 2018|newspaper=]|access-date=1 June 2020|issn=0971-751X}}</ref><ref>{{cite web|url=http://mowr.gov.in/acts-tribunals/acts/cauvery-water-management-authority-cwma|title=Cauvery Water Management Scheme, 2018|work=], ]|access-date=1 June 2024}}</ref><ref>{{Cite web|url=https://www.thenewsminute.com/article/centre-forms-9-member-cauvery-water-regulation-committee-despite-k-taka-s-opposition-83567|title=Cauvery dispute|work=News Minute|date=23 June 2018|access-date=1 June 2020}}</ref> | |||
] ] ]] | |||
== Religious significance == | |||
], Sage ] is believed to have brought Kaveri to the region.]] | |||
In ], the river is considered one of seven holy rivers in India. The river is personified and worshiped as the river goddess ''Kaveri Amman''.<ref name="Wisdom"/><ref name="Rel">{{Cite book |last=Warrier |first=Shrikala |url=https://books.google.com/books?id=qNhiCAAAQBAJ&dq=goddess+kaveri&pg=PA222 |title=Kamandalu: The Seven Sacred Rivers of Hinduism |publisher=Mayur University |year=2014 |pages=20, 192–195|isbn=978-0-95356-797-3}}</ref> Kaveri is mentioned as both a river and a goddess in various Hindu texts such as the '']'' and the '']''. The river is mentioned as one of the seven holy ] and bathing in the river is said to grant one's desired as per the '']''. The '']'' states that the river flows from the five great mountains and gives longevity to those who drink the waters of the river. The '']'' narrates the various origins of the river. ] filled ]'s ] with Kaveri, who flowed as a river with the help of ].<ref name="Wisdom"/> | |||
] | |||
] | |||
In another legend, ] becomes Agastya's wife and takes on a form of water during a severe drought in South India. Agastya carries her in his small brass water pot and Ganesha, in the form of crow, knocks the water pot down. The spilled water runs down the hill and onto the drought-stricken land.<ref>{{cite book |last=Eck |first=Diana L. |url=https://books.google.com/books?id=rNlJOSf__xYC&dq=kaveri+eck&pg=PA177 |title=India: A Sacred Geography |publisher=Harmony Books |year=2012 |location=United States |page=179|isbn=978-0-385-53191-7}}</ref> Another story narrates that during the ], or churning of the ], ] and Lopamudra retrieved the nectar of immortality for the gods. Afterwards, ] took care of Lopamudra as his daughter and later offered her to king Kavera, who renamed her as Kaveri. When Kaveri grew up she prayed to Brahma to transform her into a purifying river.<ref name="Rel"/> | |||
] | |||
] | |||
As per the ] '']'', Agastya drank the Ganges River in anger, when the floods destroyed his ] and later released it in South India. '']'' mentions Kaveri as the daughter of Kavera. In ], Kaveri is mentioned as a water channel. It is part of the twenty canal-systems associated with the reservoir Parakkamasamudda that existed in the ] region during the reign of king ].<ref name="Wisdom"/> | |||
] | |||
] | |||
== See also == | |||
] | |||
* ] | |||
] | |||
] | * ] | ||
{{SouthAsiaWaters}} | |||
== References == | |||
{{Reflist}} | |||
== External links == | |||
{{Commons category|Kaveri}} | |||
{{Kaveri River}} | |||
{{India Rivers}} | |||
{{Hydrology of Karnataka|state=collapsed}} | |||
{{Hydrography of Tamil Nadu}} | |||
{{Waters of South Asia}} | |||
{{Authority control}} | |||
] | |||
] | |||
] | |||
] | |||
] | |||
] | |||
] |
Latest revision as of 12:20, 16 December 2024
River in southern India This article is about the river. For other uses, see Kaveri (disambiguation).
Kaveri Cauvery | |
---|---|
Clockwise from top left: Talakaveri; Kaveri at Srirangapatna; Hogenakkal Falls; Kallanai Dam; Confluence with Bhavani; and Shivanasamudra Falls | |
Kaveri River basin | |
Location | |
Country | India |
Region | South India |
States | Karnataka, Tamil Nadu, Kerala, Puducherry |
Physical characteristics | |
Source | Western Ghats |
• location | Talakaveri, Kodagu district, Karnataka |
• coordinates | 12°23′N 75°29′E / 12.383°N 75.483°E / 12.383; 75.483 |
• elevation | 1,341 m (4,400 ft) |
Mouth | Bay of Bengal |
• location | Poompuhar, Mayiladuthurai district, Tamil Nadu |
• elevation | 0 m (0 ft) |
Length | 800 km (500 mi) |
Basin size | 81,155 km (31,334 sq mi) |
Discharge | |
• location | Lower Anaicut (58.5 km upstream of mouth) |
• average | 919 m/s (32,500 cu ft/s) (1998-2024) |
• minimum | 144 m/s (5,100 cu ft/s) |
• maximum | 4,075 m/s (143,900 cu ft/s) |
Discharge | |
• location | Grand Anicut (140 km upstream of mouth) |
• average | 400.716 m/s (14,151.2 cu ft/s) (1976-1979) 1,131 m/s (39,900 cu ft/s) (1998-2024) |
• minimum | 78 m/s (2,800 cu ft/s) |
• maximum | 4,916 m/s (173,600 cu ft/s) |
Basin features | |
Tributaries | |
• left | Harangi, Hemavati, Shimsha, Arkavati, Sarabanga, Thirumanimutharu |
• right | Lakshmana Tirtha, Kabini, Bhavani, Noyyal, Amaravati, Moyar |
The Kaveri (also known as Cauvery) is a major river flowing across Southern India. It is the third largest river in the region after Godavari and Krishna. The catchment area of the Kaveri basin is estimated to be 81,155 km (31,334 sq mi) and encompasses the states of Tamil Nadu, Karnataka, Kerala, and the union territory of Puducherry.
The river rises at Talakaveri in the Brahmagiri range in the Western Ghats. The source is located at an elevation of 1,341 m (4,400 ft) in the Kodagu district of Karnataka. The river flows for about 320 km (200 mi) through the Deccan plateau in Karnataka before entering Tamil Nadu. It flows further eastward in Tamil Nadu for 416 km (258 mi) before flowing into the Bay of Bengal near Poompuhar in Mayiladuthurai district of Tamil Nadu. The river flows for a total length of about 800 km (500 mi). The major tributaries include Amaravati, Arkavati, Bhavani, Hemavati, Kabini, Lakshmana Tirtha, and Noyyal.
There are a number of dams on the river which form part of an extensive irrigation system and are used for the generation of hydroelectric power. The river has supported agriculture for centuries and has served as the lifeline of several kingdoms in the past. Access to the river's waters has been a cause of dispute among the states of Karnataka and Tamil Nadu for decades. The Kaveri basin is a densely populated region, with several towns and cities located on its banks.
The river is considered as sacred by the people of Southern India and is considered to be among the seven holy rivers of India. The river is often personified and worshiped as the goddess Kaveri. The river is mentioned in various Hindu religious texts including the Mahabharata and the Puranas. In ancient Tamil literature, the river is referenced to as Ponni meaning "the golden one".
Etymology
Kaveri is mentioned in Sanskrit as a holy river in various Hindu religious texts including the Mahabharata and the Puranas. The name itself might have had different etymologies. As per Skanda Purana, the river arose after Ganesha took a form of a crow and toppled sage Agastya's kamandala. The river then took its name from the Tamil language words kā meaning "crow" and viri meaning "spread" literally translating to "spread by a crow". It might also mean a river with wide spread banks as viri can also be translated as wide spread. The etymology of the river might have also been derived from kāviri, the Sankethi word for "river" from the language spoken by the Sankethi people, who live along its waters. Cauvery is the anglicized version of the original name.
The river is also known by other names. In ancient Tamil literature, the river was called Ponni meaning "the golden one" in reference to the fine silt it deposits. It is known as Daksina gaṅgā meaning the "Ganges of the South" indicating its geographical location and its significance. It is also mentioned as Ardha gaṅgā meaning Half Ganga in Mahabharata and other literature, due to its purported mythology of having arisen from the Ganges. Marudvṛdhā is another hypothesised name for this river, meaning "the beloved of the Maruts" in Sanskrit.
Course
The river arises at Talakaveri in Kodagu district of Karnataka. The source of the river is located at an altitude of 1,341 m (4,400 ft) in the Brahmagiri Hills of the Western Ghats. Its follows a rough upper course consisting of rocky beds and high banks. Once it leaves the Kodagu hills, it flows eastwards and forms a series of rapids and falls. It flows through a narrow gorge onto the Deccan plateau and drops about 18–24 m (59–79 ft) at Chunchanakatte Falls. The river forms the island of Srirangapatna and widens to 900–1,200 ft (270–370 m) before flowing south-east. At Shivanasamudra, the river drops 91 m (299 ft) and forms 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 flowing for 320 km (200 mi) in Karnataka, the river flows for about 64 km (40 mi) along the Karnataka-Tamil Nadu border.
The river enters Tamil Nadu and forms the Hogenakkal Falls. After the falls, the river flows southwards towards Mettur Dam and joins its main right bank tributary Bhavani at Kooduthurai. The river flows eastwards through Erode and Karur, and widens further before entering the Tiruchirappalli district. It splits into two branches with the northern part called as Kollidam River and the southern part of the river retaining the name Kaveri. After flowing for 16 km (9.9 mi), the two branches converge around the Srirangam island. The river further branches off into 36 different channels before emptying into the Bay of Bengal near Puhar in Mayiladuthurai district. The river traverses for about 416 km (258 mi) in Tamil Nadu for a total length of about 800 km (500 mi).
Tributaries
The Kaveri River has 21 major tributaries. The largest tributary Hemavati, and Lakshmana Tirtha join the river at Krishna Raja Sagara. Kabini is another major contributor to the flow of Kaveri and joins the river in Karnataka. It meets with its second largest tributary Bhavani at Kooduthurai in Bhavani and two other tributaries Noyyal, and Amaravati join further down the stream in Tamil Nadu. Other tributaries of Kaveri include Shimsha, Arkavati, Sarabanga, and Thirumanimutharu.
Discharge
Source:
Year | Grand Anicut | Lower Anicut | ||||||
---|---|---|---|---|---|---|---|---|
(m/s) | (m/s) | |||||||
Min | Mean | Max | Min | Mean | Max | |||
1998 | 170 | 1,099 | 3,454 | 161 | 885 | 2,540 | ||
1999 | 289 | 1,131 | 3,778 | 285 | 864 | 2,845 | ||
2000 | 343 | 1,287 | 4,903 | 233 | 1,011 | 3,335 | ||
2001 | 258 | 1,080 | 3,348 | 309 | 948 | 3,115 | ||
2002 | 139 | 772 | 2,392 | 144 | 867 | 2,423 | ||
2003 | 78 | 667 | 2,297 | 216 | 646 | 2,100 | ||
2004 | 103 | 895 | 3,303 | 217 | 839 | 3,160 | ||
2005 | 179 | 1,012 | 3,354 | 240 | 991 | 3,873 | ||
2006 | 268 | 1,072 | 2,495 | 473 | 1,091 | 3,187 | ||
2007 | 118 | 993 | 3,308 | 324 | 1,126 | 4,075 | ||
2008 | 132 | 1,094 | 3,677 | 398 | 1,103 | 3,167 | ||
2009 | 227 | 1,040 | 3,238 | 290 | 965 | 3,301 | ||
2010 | 373 | 1,080 | 3,141 | 411 | 1,022 | 3,626 | ||
2011 | 171 | 1,163 | 3,815 | 296 | 928 | 3,014 | ||
2012 | 190 | 874 | 3,342 | 177 | 711 | 2,149 | ||
2013 | 82 | 1,043 | 3,281 | 229 | 856 | 3,127 | ||
2014 | 279 | 1,148 | 3,663 | 409 | 980 | 2,533 | ||
2015 | 559 | 1,422 | 3,816 | 407 | 913 | 2,177 | ||
2016 | 490 | 1,129 | 2,890 | 276 | 728 | 1,733 | ||
2017 | 216 | 931 | 3,586 | 154 | 671 | 1,832 | ||
2018 | 341 | 1,571 | 4,439 | 266 | 934 | 3,427 | ||
2019 | 331 | 1,473 | 4,559 | 173 | 966 | 3,070 | ||
2020 | 591 | 1,590 | 4,373 | 209 | 983 | 2,944 | ||
2021 | 478 | 1,502 | 3,935 | 257 | 988 | 3,136 | ||
2022 | 548 | 1,713 | 4,916 | 407 | 1,172 | 3,385 | ||
Overall | 78 | 1,151 | 4,916 | 144 | 928 | 4,075 |
Geology and ecology
The Kaveri basin was formed in the Late Jurassic to Early Cretaceous period during Gondwana breakup and opening of the Indian Ocean. Most of the basin is made up of Precambrian rocks and the two major rock types that are found are metamorphic and igneous rocks. Closepet granite is found in the upper parts of the Kaveri basin and Charnockite rocks are only found in the central part. A 2017 paper proposed that an impact structure was present in the vicinity of the Kaveri river. The run-off from the river does not drain off quickly because of the shape of the river basin, which limits the occurrence of floods. It is a perennial river fed mostly by monsoons. Four distinct seasons occur in the basin with hot and cold seasons sandwiching the monsoon seasons. The river basin is fed by South-West monsoon in Karnataka, and North-East monsoon in Tamil Nadu.
The Kaveri basin is made up of two sub-zones, forest and agro-ecosystem. The forest vegetation consists of a mix of dry deciduous, evergreen forests, and grasslands. As per a study, about 12,850 km (4,960 sq mi) of natural vegetation was lost in the river basin between 1965 to 2016. The basin has a variety of flora with major species including Terminalia arjuna, Tamarindus indica, Pongamia pinnata, Salix tetrasperma, Ficus benghalensis, Ficus religiosa, Eucalyptus torticornis, and Diospyros montana.
There are many protected areas spread across the river basin including significant tiger and elephant habitats. The basin provides habitat to a range of animal species such as gaur, leopard, sloth bear, Bengal tiger, Indian elephant, Nilgiri tahr, grizzled giant squirrel, and various species of deer, wild boar and reptiles. The river also hosts a variety of avifauna including the painted stork (Mycteria leucocephala), spot-billed pelican (Pelecanus philippensis), and black-headed ibis (Threskiornis melanocephalus). It is also home to the mugger crocodile (Crocodylus palustris), smooth-coated otter (Lutrogale perspicillata), and hump-backed mahseer (Tor remadevii).
Riparian zone
The total watershed of the basin is 81,155 km (31,334 sq mi) and the riparian zone of the river consists of 43,856 km (16,933 sq mi) in Tamil Nadu, 34,273 km (13,233 sq mi) in Karnataka, 2,866 km (1,107 sq mi) in Kerala, and 160 km (62 sq mi) in the union territory of Puducherry. Over half of the Kaveri basin is arable and the most cultivated crops are rice and sugarcane. An estimate at the time of the first Five Year Plan put the total flow of the river at 15 cubic kilometres (12,000,000 acre⋅ft), of which 60% was used for irrigation. The river is also used for drinking water and hydroelectric power generation.
The Grand Anicut was constructed by a Chola King in 2nd century CE. The hydroelectric plant built on the Sivanasamudra Falls in 1902 was the first hydroelectric plant in Asia. The Mettur Dam in Tamil Nadu was constructed in 1934 and the Stanley Reservoir formed by the dam has a capacity of 93.4 tmc ft. Krishna Raja Sagara in Karnataka is the second largest dam on the river and has a capacity of 49.5 tmc ft. Bhavanisagar Dam (32.8 tmc ft) on the Bhavani River in Tamil Nadu, Hemavathy Dam (37.1 tmc ft) on the Hemavathi River, Kabini Dam (18.5 tmc ft) on the Kabini River, and Harangi Dam (9.5 tmc ft) on the Harangi River in Karnataka are major dams on the tributaries of Kaveri.
Water dispute
Further information: Kaveri River water disputeThe dispute over the sharing of Kaveri waters began in 1807 when the Madras Presidency objected to the plans of the Mysore kingdom to develop irrigation projects. After initial discussions failed, the British Raj intervened and a six rule agreement called the General Agreement of 1892 was signed. After Indian Independence, article 262 of the Constitution of India provided powers to the Government of India to adjudicate on inter-state disputes on water sharing. The Government of India constituted the Cauvery Water Disputes Tribunal (CWDT) on 2 June 1990 to adjudicate the water dispute between the riparian states and territories in the river basin. In an order passed in June 1991, the CWDT directed Karnataka to release 205 tmc ft of water per year to Tamil Nadu based on a specific schedule. The water was to be released in four equal installments in a particular month and any shortfall would need to be covered in the subsequent week. Tamil Nadu was directed to provide 6 tmc ft of water to Puducherry.
In July 1991, the President of India asked the Supreme Court of India to rule on the validity and legality of the tribunal under the Constitution. In November 1991, the Supreme Court opined that the order needs to be published by the central government in the Official Gazette, which was done on 1 December 1991. In May 1992, the Government of Tamil Nadu filed a case in the Supreme Court to direct the Indian Government to pass necessary orders to ensure the implementation of the provisions of the tribunal order. In April 1997, the Attorney General of India reverted that the central government has prepared a scheme under the Inter-State Water Disputes Act, 1956 for the implementation of the tribunal award and the Cauvery Water Authority (CRA) and Cauvery Monitoring Committee (CMC) were formed subsequently as a part of the Cauvery Water (Implementation of Interim Orders of 1991 and all subsequent Tribunal Orders) Scheme, 1998. The CRA is headed by the Prime Minister of India and consists of the Chief Ministers of the riparian states as its consituent members.
On 16 February 2018, the Supreme Court ruled that 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 of water from the river. An additional 10 tmc ft was reserved for environmental protection and 4 tmc ft was reserved for wastage into the sea. The court directed the government to form a Cauvery Water Management Authority (CWMA) within six weeks and acting on the Supreme Court's direction, the central government constituted the CMWA in June 2018.
Religious significance
In Hinduism, the river is considered one of seven holy rivers in India. The river is personified and worshiped as the river goddess Kaveri Amman. Kaveri is mentioned as both a river and a goddess in various Hindu texts such as the Mahabharata and the Puranas. The river is mentioned as one of the seven holy Gangas and bathing in the river is said to grant one's desired as per the Sivapurana. The Varaha Purana states that the river flows from the five great mountains and gives longevity to those who drink the waters of the river. The Skanda Purana narrates the various origins of the river. Shiva filled Agastya's bowl with Kaveri, who flowed as a river with the help of Ganesha.
In another legend, Lopamudra becomes Agastya's wife and takes on a form of water during a severe drought in South India. Agastya carries her in his small brass water pot and Ganesha, in the form of crow, knocks the water pot down. The spilled water runs down the hill and onto the drought-stricken land. Another story narrates that during the Samudra Manthana, or churning of the Ocean of Milk, Mohini and Lopamudra retrieved the nectar of immortality for the gods. Afterwards, Brahma took care of Lopamudra as his daughter and later offered her to king Kavera, who renamed her as Kaveri. When Kaveri grew up she prayed to Brahma to transform her into a purifying river.
As per the Tamil literature Manimekalai, Agastya drank the Ganges River in anger, when the floods destroyed his tapas and later released it in South India. Silapathikaram mentions Kaveri as the daughter of Kavera. In Theravada Buddhism, Kaveri is mentioned as a water channel. It is part of the twenty canal-systems associated with the reservoir Parakkamasamudda that existed in the Polonnaruwa region during the reign of king Parakramabahu I.
See also
References
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{{cite web}}
: CS1 maint: archived copy as title (link) - Rajagopal, Krishnadas (16 February 2018). "Supreme Court curtails Tamil Nadu's share of Cauvery water". The Hindu. ISSN 0971-751X. Retrieved 1 June 2020.
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- Eck, Diana L. (2012). India: A Sacred Geography. United States: Harmony Books. p. 179. ISBN 978-0-385-53191-7.
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