page_title: Ravi River
section_title: River course
hierarchical_section_title: Ravi River / Geography / River course
caption_attribution_description: English: A view of Ravi river Lahore
context_page_description: The Ravi River is a transboundary river crossing northwestern India and eastern Pakistan. It is one of six rivers of the Indus System in Punjab region.
  Under the Indus Waters Treaty of 1960, the waters of the Ravi and two other rivers were allocated to India. Subsequently, the Indus Basin Project was developed in Pakistan, which transfers waters from western rivers of the Indus system to replenish the Ravi. Many inter-basin water transfers, irrigation, hydropower and multipurpose projects have been built in India.
context_section_description: Source reach
  The Ravi River originates in the Himalayas in the Multhan tehsil of Kangra district of Himachal Pradesh, India. It follows a north-westerly course and is a perennial river. It is the smallest of the five Punjab rivers that rises from glacier fields at an elevation of 14,000 feet (4,300 m), on the southern side of the Mid Himalayas. It flows through Barabhangal, Bara Bansu and Chamba districts. It flows in rapids in its initial reaches with boulders seen scattered in the bed of the river. The Ravi River in this reach flows in a gorge with a river bed slope of 183 feet per mile (34.7 m/km) and is mostly fed by snow melt, as this region lies in a rain shadow. Two of its major tributaries, the Budhil and Nai or Dhona join 64 kilometres (40 mi) downstream from its source. The Budhil River rises in Lahul range of hills and is sourced from the Manimahesh Kailash Peak and the Manimahesh Lake, at an elevation of 4,080 metres (13,390 ft), and both are Hindu pilgrimage sites. The entire length of Budhil is 72 kilometres (45 mi) where it has a bed slope of 314 feet per mile (59.5 m/km). It flows through the ancient capital of Bharmwar, now known as Bharmour in Himachal Pradesh. During 1858–1860, the Raja of Bharmour had considered the Budhil valley as an excellent source of Deodar trees for supply to the British Raj. However, a part of the forest surrounding the temple was considered sacred and declared a reserved area. The second tributary, the Nai, rises at Kali Debi pass, and flows for 48 kilometres (30 mi), with a bed slope of 366 feet per mile (69.3 m/km), from its source at Trilokinath to its confluence with the Ravi. This valley was also exploited for its forest wealth during the English period.
  Another major tributary that joins the Ravi River, just below Bharmour, the old capital of Chamba, is the Seul River from the northern direction. The valley formed by the river was also exploited for its rich timber trees. However, the valley has large terraces, which are very fertile and known as "the garden of Chamba". crops grown here supply grains to the capital region and to Dalhousie town and its surrounding areas. One more major tributary that joins the Ravi River near Bissoli is the Siawa. This river was also exploited for its forest resources, (controlled by the then Raja of Chamba) originating from the Jammu region. The valley is also formed by another major tributary that joins Seul River, the Baira-Nalla. Its sub-basin is in the Chamba district, located above Tissa. Baira drains the southern slopes of the Pir Panjal Range. The valley has an elevation variation between 5,321 metres (17,457 ft) and 2,693 metres (8,835 ft).
  Tant Gari is another small tributary that rises from the subsidiary hill ranges of the Pir Panjal Range east of Bharmour. The valley formed by this stream is U-shaped with a river bed scattered with boulders and glacial morainic deposits.
  Main Ravi River
  The main Ravi River flows through the base of Dalhousie hill, past the Chamba town. It is  at an elevation of 856 metres (2,807 ft) (where a long wooden bridge existed to cross the Ravi River). It flows into the south-west, near Dalhousie, and then cuts a gorge in the Dhauladhar Range, before entering the Punjab plain near Madhopur and Pathankot. It then flows along the Indo–Pak border for 80 kilometres (50 mi) before entering Pakistan and joining the Chenab River. The total length of the river is about 725 kilometres (450 mi).
  Ujh River is another major tributary of the Ravi River. Its source is in the Kailash mountains at an elevation of 4,300 metres (14,100 ft), close to the Bhaderwah Mountains in Jammu district. After flowing for 100 kilometres (62 mi), it joins Ravi at Nainkot in Pakistan.
  As the Ravi flows past Lahore in Pakistan (26 kilometres (16 mi) below Amritsar in India) it is called "The river of Lahore" since that city is on its eastern bank. After passing through Lahore the river takes a turn at Kamalia and then debouches into the Chenab River, south of the town of Ahmadpur Sial. On its western bank is the town of Shahdara Bagh 
caption: Boats floating beside the Ravi River in Lahore
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