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This is an accepted version of this page This is the latest accepted revision, reviewed on 28 January 2025. River in Asia "Indus Valley" redirects here. For the Bronze Age civilisation, see Indus Valley Civilisation. For other rivers named Indus, see Indus (disambiguation) § Rivers. "Indus" and "Sindhu" redirect here. For other uses, see Indus (disambiguation) and Sindhu (disambiguation ...
The Sutlej River [a] is a major river in Asia, flowing through China, India and Pakistan, and is the longest of the five major rivers of the Punjab region. It is also known as Satadru; [3] and is the easternmost tributary of the Indus River. The combination of the Sutlej and Chenab Rivers forms the Panjnad, which finally flows into the Indus River.
English: Map of the Indus River basin with tributaries labeled. Yellow regions are non-contributing parts of the watershed (e.g. the Thar Desert). Date: 2 February 2018:
The Himalayan watershed is the source of majority of the major river systems in India including the three longest rivers–the Ganges, the Brahmaputra and the Indus. [3] [4] These three river systems are fed by more than 5000 glaciers. [5]
The Indus Basin. The Indus Basin is the part of Asia drained by the Indus River and its tributaries. The basin covers an area of 1,120,000 km 2 (430,000 sq mi) [1] [a] traversing four countries: Afghanistan, China, India, and Pakistan, with most of the area lying predominantly in the latter two countries.
Indus: Síndhu – Identified with Indus. [5] The central lifeline of RV. [6] Northwestern Rivers: Tr̥ṣṭā́mā – Blažek identifies with Gilgit. [5] Witzel notes it to be unidentified. [1] Susártu – Unidentified. Ánitabhā – Unidentified. Rasā́ – Described once to be on the upper Indus; at other times a mythical entity. [5]
The Ravi River, a transboundary river of India and Pakistan, is an integral part of the Indus River Basin and forms the headwaters of the Indus basin. The waters of the Ravi River drain into the Arabian Sea (Indian Ocean) through the Indus River in Pakistan. The river rises in the Bara Bhangal, Kangra District in Himachal Pradesh, India. The ...
Recent geophysical research shows that the supposed downstream Ghaggar-Hakra paleochannel is actually a paleochannel of the Sutlej, which flowed into the Nara river, a delta channel of the Indus River. Around 10,000-8,000 years ago, this channel was abandoned when the Sutlej diverted its course, leaving the Ghaggar-Hakra as a system of monsoon ...