major river groups of india

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    Major river groups of India

    Based on the topography, the river systems of India can be classified into four groups. These are:

    Himalayan Rivers Deccan Rivers Coastal Rivers Rivers of the Inland Drainage Basin

    The Himalayan Rivers

    The Himalayan Rivers receive input from rain as well as snowmelt and glacier melt and, therefore,have continuous flow throughout the year. During the monsoon months of June to September,

    Himalayas receive very heavy rainfall and experience maximum snow melt and these are the periods

    when the rivers carry about 80% or more of the annual flows. This is also the time when these rivers

    are prone to flooding.

    The main river systems in Himalayas are those of the Indus and the Ganga-Brahmaputra-Meghna.

    The Indus rises near Mansarovar in Tibet. Flowing through Kashmir, it enters Pakistan and finally

    falls in the Arabian Sea near Karachi. A number of important tributaries of Indus flow through India,

    namely, the Sutlej, the Beas, the Ravi, the Chenab and the Jhelum.

    Bhagirathi and Alakhnanda are two important rivers that originate in Garhwal Himalayas. These join

    at Devprayag to form Ganga which is the most sacred river of India. This river traverses through

    Uttaranchal, Uttar Pradesh, Bihar, and West Bengal and thereafter enters Bangladesh. The important

    tributaries of Ganga are the Yamuna, the Ramganga, the Ghaghra, the Gandak, the Kosi, and the

    Sone. Many of these tributaries are mighty rivers themselves. Yamuna River is an important tributary

    of Ganga and its own important tributaries are Chambal and Betwa.

    The Brahmaputra rises in Tibet where it is known by the name Tsangpo. It enters India in Arunachal

    Pradesh and after traversing through Assam, enters Bangladesh. Its important tributaries are the

    Dibang, Lohit, Subansiri, Manas and Teesta. Ganga and Brahmaputra rivers meet at Goalundo inBangladesh. The Barak River, the head stream of Meghna rises in the hills in Manipur. The Meghna

    is the part of Ganga-Brahmaputra-Meghna-System. The combined Ganga-Brahmaputra River meets

    Meghna in Bangladesh and their huge volume of water flows into the Bay of Bengal.

    Harnessing the waters of the major rivers that flow from the Himalayas is of paramount importance

    for India, Nepal, and Bangladesh. Through a close collaboration and pooling resources, huge benefits

    can be realized from flood control, assured irrigation, hydroelectric power generation, employment

    generation, and improvement of environmental quality. As these countries grapple with the political

    compulsions and realities, both domestic and international, of utilizing the flow of the Ganga-

    Brahmaputra system, precious water, largely unutilized, continues to flow to the sea. At times, it also

    inflicts large losses to life and property.

    Principal Himalayan rivers of India

    Group

    No.Order of magnitude (Area in km2) Name of river Himalayan area included in

    catchment (km2)

    I Above 256,000 Indus 265,728

    II Between 128,000 and 256,000 Brahmaputra 253,952

    III Between 38,400 and 128,000 Kosi 61,184

    Karnali 52,736

    Satluj 47,360

    IV Between 25,600 and 38,400 Gandak 37,376

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    e um ,

    Manas 30,720

    Chenab 26,880

    Raidak 26,112

    V Between 12,800 and 25,600 Ganga 22,784

    Luhit 20,480

    Subansiri 17,920

    Kali 16,128

    Beas 14,336

    Dibang 12,800

    VI Below 12,800 Tista 12,288

    Yamuna 11,520

    Ravi 7,936

    Rapti 7,680

    Ramganga 6,656

    Baghmati 3,840

    The Deccan Rivers

    The rivers of Deccan can be further classified in two groups: west flowing rivers and east flowing

    rivers. The Narmada and the Tapi rivers flow westwards into Arabian Sea. The important east

    flowing rivers are the Brahmani, the Mahanadi, the Godavari, the Krishna, the Pennar, and the

    Cauvery. These rivers fall into the Bay of Bengal.

    The Mahanadi, rising in the state of Madhya Pradesh, is an important river in the state of Orissa. In

    the upper drainage basin of Mahanadi, which is centered on the Chhattisgarh Plain, periodic droughts

    contrast with the situation in the delta region where floods damage the crops in the rice bowl ofOrissa. Hirakud Dam, constructed in the middle reaches of Mahanadi, has helped in alleviating these

    adverse effects to a large extent by creating a reservoir.

    The source of the Godavari is near Nasik, northeast of Mumbai (Bombay) in the state of

    Maharashtra, and the river follows a southeasterly course for 1,400 kilometers (km) to its mouth on

    the Andhra Pradesh coast. The Godavari basin is second in size only to Ganga; its delta on the east

    coast is also one of the country's main rice-growing areas. It is known as the Ganga of the South but

    despite the large catchment area, its discharge is moderate. The reason is medium depth of annual

    rainfall, for example, about 700 mm at Nasik and 1,000 mm at Nizamabad.

    The Krishna rises in the Western Ghats and flows east into the Bay of Bengal. Its flow is not very

    large because of low rainfall in its catchment area: 660 mm annually at Pune. The Krishna is the third

    longest river in India.

    The source of the Cauvery is in the state of Karnataka and the river flows southeastward. Its main

    tributaries are the Bhima, the Tungabhadra, the Ghatprabha and the Malaprabha. The waters of the

    river have been a source of irrigation since antiquity; in the early 1990s, an estimated 95% of the

    Cauvery flow was diverted for agricultural use.

    The Narmada and the Tapi are the only major rivers that flow eastward into the Arabian Sea. The

    Narmada rises in Madhya Pradesh and crosses the state, passing swiftly through a narrow valley

    between the Vindhya Range and spurs of the Satpura Range. It flows into the Gulf of Khambhat (or

    Cambay). Tapi which is of shorter length follows a generally parallel course, between 80 km and 160

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    ,

    way into the Gulf of Khambhat.

    The Coastal Rivers

    There are numerous coastal rivers which are comparatively small. While only handful of such rivers

    drain into the sea near the deltas of east coast, there are as many as 600 such rivers on the west

    coast. The West Coast rivers are important as they contain as much as 14% of the countrys water

    resources while draining only 3% of the land.

    Rivers of the Inland Drainage Basin

    The rivers of the inland system, centered in western Rajasthan state, are few and frequently

    disappear in years of scant rainfall. A few rivers in Rajasthan do not drain into the sea. They drain

    into salt lakes or get lost in sands with no outlet to sea.