Indian River and Its Tributeries Essay

The Lohit River has derived its name because of its vigorous nature and thusly it is besides called the river of blood. The lateritic soil of the river forms its surrounding demography. The river runs with the Mishmi Hills, to meet the Siang at the head of the Brahmaputra valley. The Burhidihing River is 1 of the major tributaries of the Brahmaputra River. The River Burhidihing stream at the race of 103. 58m at Khowang. The urines fall from an upbringing of 102. 11m. This river is broad(prenominal)ly pr wiz to startpourings and the previous highest flood direct was measured to be 103. 92m in1988.decameterodar River-The Damodar River originates in the Palamau regularise of Jharkhand go up Chandwa village. The origin of Damodar River is in the Chota Nagpur Plateau region of India. The river flows finished the states of Jharkhand and western hemisphere Bengal for nearly five hundred and ninety two kilometers and then merges with the Hooghly River, which is in the con su pplyeration west of Kolkata. The Damodar River has a number of tributaries and distributaries. They ar Barakar, Konar, Guaia,Jamania, Usri, Bokaro, Haharo, Khadia and Bhera. The Barakar is the most important and the only bird feeder of the Damodar River.This River arises near Padma in Hazaribagh district, flows through Jharkhand,and meets the Damodar River in Dishergarh in western united States Bengal. The river used to flow through Bengal in yesteryears, from west to atomic number 99 line of descent and then it joined the Hooghly River at a spot near Kalna. Gradually, the river has changed its scarper and now most of the water in its lower reaches falls into the Mundeswari River. The Mundeswari River combines with other rivers and ultimately most of the water of the Damodar River flows into the Rupnarayan River. The residual water flows through the Damodar into the Hooghly, located at the atomic number 16 of Kolkata.Earlier the Damodar River was referred to as River of So rrow in Bengal as it used to flood the Bardhaman, Hooghly, Howrah and Medinipur districts of West Bengal, which led to huge destruction of life-time and property. Even today the floods sometimes damage the lower Damodar Valley but the snake pit it brought intimately in earlier years. However, afterwards move oning the dams this flood factor has require a matter of history. Pollution of Damodar River is unmatchable of the grave concerns of the Bengal authorities. The Damodar is the most polluted river in India today due the several industries that live sprouted on its mineral-rich banks.There are too many scorch- ground industries that are been build the Damodar valley. Other industries are mostly government-owned char washeries, coke oven plants, which are the countrys major iron and steel plants and caloric index plants. Zinc, glass and cement plants also cover wide areas along the riverbanks. The saddle of mine effluents, fly ash, oil, toxic surfaces and coal dust c aused the defilement. Defective mining practices, over-the-hill processing practices and lack of proper charge were compounded by corruption, inadequate contamination control and a state pollution control board that did nothing.The people active in the basin are late being pois wizd because the Damodar and its tributaries is the only source of drinkable water for most people reenforcement in the area. However, the governmental measures have brought world-shaking changes in the status of the river for the past years. The geology of Damodar River intimate heavy metal concentrations at divers(a) zones of the river. At two sites in near mining areas, the coarser disrupticles show similar or even higher heavy metal concentrations than the finer ones. Damodar Valley Corporation (DVC) is based on the Tenesse Valley Authority of the United States of America.This project benefits the states of West Bengal and Bihar. An important mark of this project is the 692 metres long and 11. 6 metres high barrage constructed crosswise the Damodar at Durgapur. Panchet dam, Farakka Barrage, Tilaiya Dam and Konar Dam are the dams at River Damodar. The secondary of Damodar River is one of the most ferocious and big rivers of Eastern India River Barakar, which begins near Padma in Hazaribagh district of Jharkhand and flows for 225 km across the couplingern part of the Chota Nagpur plateau.GANGA The aggroup River is held spiritual by Hindus and is revere in its personified formas the Goddess Ganga. The Ganga and its tributaries drain a jumbo and fertile basin with an area of about one million square kilometres. The aggroup has a number of tributaries which are mentioned on a lower floor Yamuna River Yamuna River, also known as the Jumna, is a major river of the northwestern India. Yamuna River has a union length of about 1,376 km (855 mi). The Yamunas source is at the Yamunotri glacier near Banderpoonch peaks, in the Mussourie aim of the lower Himalayas at an fo stering of about 6387 meters above sea level in district Uttarakashi.This river, flows in a southerly armorial bearing through the Himalayan foothills, onto the northern Indian plain, and a serial of valleys for about 200Kms, along the Uttar Pradesh-Haryana state clay sculpture. At this point, the Eastern and Western Yamuna canals are fed from the river. Son River One of the largest southern tributaries of the gang up is the Son River of central India. The Son River originates in the state of Chhattisgarh in the east direction of the origin of Narmada River. It then flows in the nor-nor-west direction through Madhya Pradesh before round in the east direction where it meets the Kaimur range.The river starts flowing in the parallel direction of the Kaimur range in the east-northeast direction through Uttar Pradesh and Bihar and joins the Ganges just above Patna, the capital of Bihar. Mahananda River The Mahananda River is a major confluent of the Ganges in eastern part of India. The river originates from the extreme north of West Bengal from thehills of Darjeeling. It then flows southwards through the fertile agricultural area I in Bihar and enters West Bengal. The river then flows in the southeast direction I in to Bangladesh.I Kosi River I Kosi River one of the main rivers in Bihar and a prominent eater of the Ganges, originates in the Himalayas. Along with its tributaries, the Kosi River traverses along move of Tibet, including the Mount Everest region and also one third of the eastern part of Nepal. The river has shifted its course from east to west about cxx kilometres in the last two hundred years. Gandak River Gandak is also known as the samphire Gandaki River and Narayani after the confluence with Trisuli in Nepal. Gandak River is a tributary of the Ganga or Ganges River.It is one of the major rivers in Nepal and India. It is a north bank tributary of the Ganga in India. It rises at 7620 m in Tibet near the Nepal modelling and overlooks the D haulagiri. It is distinguished for the deep gorge across which it flows and for a large hydroelectric deftness in Nepal. This river also provides water for a major Irrigation cum Hydroelectric power facility at the Indo-Nepal border at Valmikinagar. The river has a total catchment area of 46,300 sqkm out of which 7620 sqkm is located in India. The Gandaki River is mentioned in the old-fashioned Indian epic Mahabharata.Ghaghara River Ghaghara River, also called the Gogra or Ghagra, Nepali Kauriala or Manchu or the Karnali, literally convey holy water from the sacred mountain. The term Karnali also means Turquoise River and is a trans-boundary perennial river that originates on the Tibetan plateau. The Karnali is called Kung-chiao Ho in Chinese. This river near Manasarowar cuts through the Himalayas in Nepal on its way to the convergence with the Sarda River at Brahmaghat in India where it forms the Ghaghara River. The Ghaghara River is a major go forth bank tributary of the Gange s.It is the longest and largest river in Nepal with a length of around 507 km and one of the largest affluent of the Ganges. Mahakali River River Mahakali flows surrounded by the border of Nepal and India. This river forms the western international border between Nepal and India and it originates from the Greater Himalayas at Kalapaani. The river flows down from a height of 3600 m, in the Pithoragarh District of Uttarakhand. Eventually, it joins with the Gori Ganga at Jauljibi area. This river again joins the Saryu River at Pancheshwar. The vicinity