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The Chenab River is a major river in and , and one of the five major rivers associated with the region. It is formed by the union of two headwaters, the Chandra and Bhaga, which rise in the upper in the Lahaul region of , India. The Chenab then flows through the of Jammu and Kashmir, India, into the plains of Punjab, Pakistan, where it joins the to form the , which ultimately flows into the at .

The waters of the Chenab were allocated to Pakistan under the terms of the Indus Waters Treaty. India is allowed non-consumptive uses such as power generation. The Chenab River is extensively used in Pakistan for irrigation. Its waters are also transferred to the channel of the via numerous link canals.


Name
The Chenab river was called () in the (VIII.20.25, X.75.5). The name meant that it was seen to have dark-coloured waters. The term Krishana is also found in the . A later form of Askikni was Iskamati () and the Greek form was – Akesínes; Latinized to Acesines.

In the , the common name of the river was Chandrabhaga () because the river is formed from the confluence of the Chandra and the Bhaga rivers. This name was also known to the Ancient Greeks, who Hellenised it in various forms such as Sandrophagos, Sandabaga and Cantabra.

The simplification of Chandrabhaga to 'Chenab', with evident Persianate influence, probably occurred in early medieval times and is witnessed in .


Course

Present course
The river is formed by the confluence of two rivers, Chandra and Bhaga, at Tandi, southwest of , in the Lahaul and Spiti district of the state of .

The Bhaga River originates from lake, which is situated a few kilometers west of the pass in Himachal Pradesh. The Chandra River originates from glaciers east of the same pass (near ).

This pass also acts as a water-divide between these two rivers.

The Chandra river transverses while the Bhaga river transverses through narrow gorges before their confluence at Tandi.

The Chandra-Bhaga then flows through the of in Himachal Pradesh before entering the Jammu division of Jammu and Kashmir, where it flows through the Kishtwar, , , and . It enters Pakistan and flows through the Punjab province before emptying into the Sutlej, forming the .


Historical course
Historically, the Chenab River used to flow east of Multan prior to 1245, after which the Beas River occupied its old bed that went by Dipalpur. The Jhelum, Chenab, and Ravi rivers met in the northeastern direction of Multan, then flowing east together until they met the Beas River near Uchh in the southern direction of Multan. However, by 1397 the flow of the Chenab River shifted so that it flows west of Multan.


History
The river was known to Indians in the Vedic period. In 325 BCE, Alexander the Great allegedly founded the town of Alexandria on the Indus (present-day Uch Sharif or Mithankot or Chacharan in Pakistan) at the confluence of the Indus and the combined streams of Punjab rivers (currently known as the ). , in the Anabasis of Alexander, quotes the eyewitness as writing that the river was wide where Alexander crossed it.
(2025). 9780375423468, . .

The Battle of Chenab was fought between and on the bank of the river.


Dams
The river has rich power generation potential in India. There are many dams built, under construction or proposed to be built on the Chenab for the purpose of hydroelectric power generation in the country, including:

All of these are "run-of-the-river" projects as per the Indus Water Treaty of 1960. The Treaty allocates the waters of Chenab to Pakistan. India can use its water for domestic and agricultural uses or for "non-consumptive" uses such as . India is entitled to store up to of water in its projects. The three projects completed , Salal, Baglihar and Dul Hasti, have a combined storage capacity of .

Pakistan has four headworks on the Chenab:


See also

Notes

Bibliography


External links
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