List of major rivers of India
The rivers of India play an important role in the lives of the Indian people. The river systems provide irrigation, potable water, cheap transportation, electricity, as well as provide livelihoods for a large number of people all over the country. This easily explains why nearly all the major cities of India are located by the banks of rivers. The rivers also have an important role in Hindu mythology and are considered holy by all Hindus in the country.
Seven major rivers along with their numerous tributaries make up the river system of India. Most of the rivers pour their waters into the Bay of Bengal. Some of the rivers whose courses take them through the western part of the country and towards the east of the state of Himachal Pradesh empty into the Arabian Sea. Parts of Ladakh, northern parts of the Aravalli range and the arid parts of the Thar Desert have inland drainage. All major rivers of India originate from one of the three main watersheds.
- The Himalaya and the Karakoram ranges
- Vindhya and Satpura ranges and Chotanagpur plateau in central India
- Sahyadri or Western Ghats in western India
Classification
The rivers of India can be classified on the basis of origin and on the type of basin that they form
On the basis of origin
On the basis of origin, the rivers of India can be divided into Himalayan rivers and Peninsular rivers.
''''Himalayan rivers''''
The main Himalayan river systems are the Ganga, the Indus and the Brahmaputra river systems.
The Himalayan rivers form large basins. Many rivers pass through the Himalayas. These deep valleys with steep rock sides were formed by the down - cutting of the river during the period of the Himalayan uplift. They perform intense erosional activity up the streams and carry huge load of sand and silt. In the plains, they form large meanders, and a variety of depositional features like flood plains, river cliffs and levees.
These rivers are perennial as they get water from the rainfall as well as the melting of ice. Nearly all of them create huge plains and are navigable over long distances of their course. These rivers are also harnessed in their upstream catchment area to generate hydroelectricity.
Peninsular rivers
The main peninsular river systems include the Narmada, the Tapi, the Godavari, the Krishna, the Kaveri and the Mahanadi river systems.
The Peninsular rivers flow through shallow valleys. A large number of them are seasonal as their flow is dependent on rainfall. The intensity of erosional activities is also comparatively low because of the gentler slope. The hard rock bed and lack of silt and sand does not allow any significant meandering. Many rivers therefore have straight and linear courses. These rivers provide huge opportunities for hydro-electric power.
The Indus originates in the northern slopes of the Kailash range in Tibet . It enters Indian territory in Jammu and Kashmir. . Several tributaries - the Zaskar, the Shyok, the Nubra and the Hunza join it in the Kashmir region. It flows through the regions of Ladakh, Baltistan and Gilgit and runs between the Ladakh Range and the Zaskar Range. It crosses the Himalayas through a 5181 m deep gorge near Attock, lying north of the Nanga Parbat and later takes a bend to the south west direction before entering Pakistan.
Jhelum
The Jhelum originates in the south-eastern part of Kashmir, in a spring at Verinag.
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Chenab
The Chenab originates from the confluence of two rivers, the Chandra and the Bhaga, which themselves originate from either side of the Bara Lacha Pass in Lahul. It is also known as the Chandrabhaga in Himachal Pradesh. It runs parallel to the Pir Panjal Range in the north-westerly direction, and cuts through the range near Kishtwar. It enters the plains of Punjab near Akhnur and is later joined by the Jhelum. It is further joined by the Ravi and the Sutlej in Pakistan.
Ravi
The Ravi originates near the Rotang pass in the Kangra Himalayas and follows a north-westerly course. It turns to the south-west, near Dalhousie, and then cuts a gorge in the Dhaola Dhar range entering the Punjab plain near Madhopur. It flows as a part of the Indo-Pakistan border for some distance before entering Pakistan and joining the Chenab river. The total length of the river is about 720 km.This river is of great significance in terms of hydroelectricity generated.on this river we there is hydroelectric project called as chamera hydroelectric project producing 540 MW of electricity.the dam is at chohra and powerhouse is at khairi.and one another dam ranjeet sagar dam is also located on this river.Khairi is a township on the river side which is 30 kms away from banikhet and a house to NHPC employees invoved in electricity generation in 540 mw plant .kendriya vidyalaya is also located in the place for schooling of the childern of nhpc employees.
Beas
The Beas originates in Beas Kund, lying near the Rohtang pass. It runs past Manali and Kulu, where its beautiful valley is known as the Kulu valley. It first follows a north-west path from the town of Mandi and later a westerly path, before entering the Punjab plains near Mirthal. It joins the Sutlej river near Harika, after being joined by a few tributaries. The total length of the river is 615 km.
Sutlej
The Sutlej originates from the Rakas Lake, which is connected to the Manasarovar lake by a stream, in Tibet. Its flows in a north-westerly direction and enters Himachal Pradesh at the Shipki Pass, where it is joined by the Spiti river. It cuts deep gorges in the ranges of the Himalayas, and finally enters the Punjab plain after cutting a gorge in a hill range, the Naina Devi Dhar, where the Bhakra Dam having a large reservoir of water, called the Gobind Sagar, has been constructed. It turns west below Rupar and is later joined by the Beas. It enters Pakistan near Sulemanki, and is later joined by the Chenab. It has a total length of almost 1500 km.
The Brahmaputra River System
The Brahmaputra originates in the Mansarovar lake, also the source of the Indus and the Satluj. It is slightly longer than the Indus, but most of its course lies outside India. It flows eastward, parallel to the Himalayas. Reaching Namcha Barwa (7757 m), it takes a U-turn around it and enters India in Arunachal Pradesh and known as dihang. The undercutting done by this river is of the order of 5500 metres. In India, it flows through Arunachal Pradesh and Assam, and is joined by several tributaries.
In Tibet, the river is known as the Tsangpo. There, it receives less volume of water and has less silt. But in India, it passes through a region of heavy rainfall and as such, the river carries a large amount of rainfall and considerable amount of silt. The Brahmaputra has a braided channel throughout most of its length in Assam, with a few large islands within the channel.
The shifting of the channels of the river is also very common. The fury of the river during rains is very high. It is known for creating havoc in Assam and Bangladesh. At the same time, quite a few big pockets suffer from drought.
The Narmada River System
The Narmada or Nerbudda is a river in central India. It forms the traditional boundary between North India and South India, and is a total of 1,289 km (801 mi) long. Of the major rivers of peninsular India, only the Narmada, the Tapti and the Mahi run from east to west. It rises on the summit of Amarkantak Hill in Madhya Pradesh state, and for the first 320 kilometres (200 miles) of its course winds among the Mandla Hills, which form the head of the Satpura Range; then at Jabalpur, passing through the 'Marble Rocks', it enters the Narmada Valley between the Vindhya and Satpura ranges, and pursues a direct westerly course to the Gulf of Cambay. Its total length through the states of Madhya Pradesh, Maharashtra, and Gujarat amounts to 1312 kilometres (815 miles), and it empties into the Arabian Sea in the Bharuch district of Gujarat.
The Tapti River System
Tapti River
The Tapti is a river of central India. It is one of the major rivers of peninsular India with the length of around 724 km, and only the Tapi River along with the Narmada river, and the Mahi River run from east to west. It rises in the eastern Satpura Range of southern Madhya Pradesh state, and flows westward, draining Madhya Pradesh's historic Nimar region, Maharashtra's historic Khandesh and east Vidarbha regions in the northwest corner of the Deccan Plateau and South Gujarat before emptying into the Gulf of Cambay of the Arabian Sea, in the State of Gujarat. The Western Ghats or Sahyadri range starts south of the Tapti River near the border of Gujarat and Maharashtra.
The Tapti River Basin lies mostly in northern and eastern districts Maharashtra state viz, Amravati, Akola, Buldhana, Washim, Jalgaon, Dhule, Nandurbar, Malegaon, Nashik districts but also covers Betul, Burhanpur districts of Madhya Pradesh and Surat district in Gujarat as well.
The principal tributaries of Tapi River are Purna River, Girna River, Panzara River, Waghur River, Bori River and Aner River.
The Godavari River System
Main article : Godavari River
The river with second longest course within India, Godavari is often referred to as the Vriddh (Old) Ganga or the Dakshin (South) Ganga. The name may be apt in more ways than one, as the river follows the course of Ganga's tragedy. The river is about 1,450 km (900 miles) long. It rises at Trimbakeshwar, near Nasik and Mumbai (formerly Bombay) in Maharashtra around 380 km distance from the Arabian Sea, but flows southeast across south-central India through the states of chhattisgarh, and Andhra Pradesh, and empties into the Bay of Bengal. At Rajahmundry, 80 km from the coast, the river splits into two streams thus forming a very fertile delta. Like any other major rivers in India, the banks of this river also has many pilgrimage sites, Nasik, Triyambak and Bhadrachalam, being the major ones. It is a seasonal river, widened during the monsoons and dried during the summers. Godavari river water is brownish. Some of its tributaries include Indravati River, Pranahita (Combination of Penuganga and Warda), Manjira, Bindusara and Sabari kinnerasani. Some important urban centers on its banks include Nasik, Bhadrachalam, Rajahmundry and Narsapur. The Asia's largest rail-come-road bridge on the river Godavari linking Kovvur and Rajahmundry is considered to be an engineering feat.
The Krishna River System
The Krishna is one of the longest rivers of India (about 1300 km in length). It originates at Mahabaleswar in Maharashtra and meets the sea in the Bay of Bengal at Hamasaladeevi in Andhra Pradesh. The Krishna River flows through the states of Maharashtra, Karnataka and Andhra Pradesh.
The traditional source of the river is a spout from the mouth of a statue of a cow in the ancient temple of Mahadev in Mahabaleshwar.
Its most important tributary is the Tungabhadra River, which itself is formed by the Tunga and Bhadra rivers that originate in the Western Ghats. Other tributaries include the Koyna, Bhima, Mallaprabha, Ghataprabha, Yerla, Warna, Dindi, Musi and Dudhganga rivers.as
The Kaveri River System
The Kaveri (also spelled Cauvery or Kavery) is one of the great rivers of India and is considered sacred by the Hindus. This river is also called Dakshin Ganga. The headwaters are in the Western Ghats range of Karnataka state, and from Karnataka through Tamil Nadu. It empties into the Bay of Bengal. Its waters have supported irrigated agriculture for centuries, and the Kaveri has been the lifeblood of the ancient kingdoms and modern cities of South India.
The source of the river is Talakaveri located in the Western Ghats about 5,000 feet (1,500 m) above sea level. Talakaveri is a famous pligrimage and tourist spot set amidst Bramahagiri Hills near Madikeri in Kodagu district of Karnataka. Thousands of piligrims flock to the temple at the source of the river especially on the specified day known as Tula sankramana when the river water has been witnessed to gush out like a fountain at a predetermined time. It flows generally south and east for around 765 km, emptying into the Bay of Bengal through two principal mouths. Its basin is estimated to be 27,700 square miles (71,700 km2), and it has many tributaries including Shimsha, Hemavati River, Arkavathy, Kapila, Honnuhole, Lakshmana Tirtha, Kabini, Lokapavani, Bhavani, Noyyal and Famous Amaravati.
The Mahanadi River System
Mahanadi River Delta in India is a basin of deposit that drains a large land mass of the Indian subcontinent into the Bay of Bengal. The alluvial valley is wide and relatively flat with a meandering river channel that changes its course.[1]
The Mahanadi River flows slowly for 560 miles (900 km) and has an estimated drainage area of 51,000 square miles (132,100 square km). It deposits more silt than almost any other river in the Indian subcontinent.[2]
The area of the drainage basin is 141,464 km². The interior coastal plain has a relatively low elevation. The average elevation of the drainage basin is 426 m, with a maximum of 877 m and a minimum of 193 m.
Rivers in Mythology
Ganga
The Ganga is personified in Hinduism as a goddess: Maa Ganga (Mother Ganga). Hindu legend makes her the foster-mother of Karttikeya, who was actually a son of Shiva and Parvati. Several places sacred to Hindus lie along the banks of the river Ganga, including Haridwar and Varanasi. It is believed that taking a dip in the river will wash away one's sins, and that having one's ashes disposed of in the Ganga after death may greatly improve one's next life or even allow Moksha to be attained sooner. Devout Hindus make pilgrimages to bathe in the Ganga and to meditate on its banks.
According to mythological legend, Brahma collected the sweat of Vishnu's feet and created Ganga. Being touched by two members of the Trimurti, Ganga became very holy.
Several years later, a king named Sagara magically acquired sixty thousand sons. One day, King Sagara performed a ritual of worship for the good of the kingdom. One of the integral parts of the ritual was a horse, which was stolen by the jealous Indra. Sagara sent all his sons all over the earth to search for the horse. They found it in the nether-world (or Underworld) next to a penitent sage Kapila. Believing that the sage had stolen the horse, they hurled insults at him and caused his penance to be disturbed. The sage opened his eyes for the first time in several years, and looked at the sons of Sagara. With this glance, all sixty thousand were burnt to death. The souls of the sons of Sagara wandered as ghosts since their final rites had not been performed. When Bhagiratha, one of the descendants of Sagara, son of Dilip, learnt of this fate, he vowed to bring Ganga down to Earth so that her waters could cleanse their souls and release them to heaven.
Bhagiratha prayed to Brahma that Ganga come down to Earth. Brahma agreed, and he ordered Ganga to go down to the Earth and then on to the nether regions so that the souls of Bhagiratha's ancestors would be able to go to heaven. The vain Ganga felt that this was insulting and decided to sweep the whole earth away as she fell from the heavens. Alarmed, Bhagiratha prayed to Shiva that he break up Ganga's descent.
Ganga arrogantly fell on Shiva's head. But Shiva calmly trapped her in his hair and let her out in small streams. The touch of Shiva further sanctified Ganga. As Ganga travelled to the nether-worlds, she created a different stream to remain on Earth to help purify unfortunate souls there.
Because of Bhagiratha's efforts Ganga descended on to earth and hence the river is also known as Bhagirathi, and the term "Bhagirath prayatna" is used to describe valiant efforts or difficult achievements.
Another name that Ganga is known by is Jahnavi. Story has it that once Ganga came down to earth, on her way to Bhagiratha, her rushing waters created turbulence and destroyed the fields and the sadhana of a sage called Jahnu. He was angered by this and drank up all of Ganga's waters. Upon this, the Gods prayed to Jahnu to release Ganga so that she could proceed on her mission. Pleased with their prayers, Jahnu released Ganga (her waters) from his ears. Hence the name "Jahnavi" (daughter of Jahnu) for Ganga.
Ganga is also called the mother of 'Bhishma Pitamah'.
Yamuna
According to legend the goddess of the river is the sister of the Hindu god of death, Yama and the daughter of Surya, the Sun god. The river Yamuna is also connected to the mythology surrounding the Hindu god Krishna.
Narmada
In sanctity the Narmada ranks only second to the Ganges among the rivers of India in Hindu religion, and along its whole course are special places of pilgrimage, including Maheshwar in Madhya Pradesh. The most meritorious act that a pilgrim can perform is to walk from the sea to the source of the river and back along the opposite bank. This pilgrimage takes from one to two years to accomplish.
The Narmada is closely associated with Lord Shiva. Naturally formed smooth stones called banas, made of cryptocrytalline quartz, are found in Narmada which are known as Shivalingas; the rare and unique markings on them are regarded by shaivaites as very auspicious. The Brihadeeswara Temple in Thanjavur, Tamil Nadu, constructed by Rajaraja Chola, has one of the biggest Bana Shivalingas. Adi Shankara met his guru Govinda Bhagavatpada on the banks of river Narmada.
Kaveri
The Kaveri is known to devout Hindus as Dakshina Ganga, or the Ganges 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 Brahma; 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 underground once in the year to the source of the Cauvery, to purge herself from the pollution contracted from the crowd of sinners who have bathed in her waters.