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This is an accepted version of this page This is the latest accepted revision, reviewed on 15 December 2024. 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 ...
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 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.
The Indus River Delta forms where the Indus River flows into the Arabian Sea, mostly in the southern Sindh province of Pakistan with a small portion in the Kutch Region of India. The delta covers an area of about 41,440 km 2 (16,000 sq mi), and is approximately 210 km (130 mi) across where it meets the sea.
Indus Valley Civilisation Alternative names Harappan civilisation ancient Indus Indus civilisation Geographical range Basins of the Indus river, Pakistan and the seasonal Ghaggar-Hakra river, eastern Pakistan and northwestern India Period Bronze Age South Asia Dates c. 3300 – c. 1300 BCE Type site Harappa Major sites Harappa, Mohenjo-daro, Dholavira, and Rakhigarhi Preceded by Mehrgarh ...
Located in Sindh, Pakistan, on the banks of the Indus River. With no citadel, it is merely an Indus site. Excavated items include bronze statues of bullock carts and ekkas as well as a small jar that appears to be a kink well. Bead making factory, dockyard, button seal, fire altars, painted jar, earliest cultivation of rice (1800 BC) Manda, Jammu
Multiple hydronyms are located in the Rigvedic corpus; they are slotted according to rough geographical locations, following the scheme of Michael Witzel. [1] Alongside, opinions of scholars about modern correlates are provided: [5] [6] Indus: Síndhu – Identified with Indus. [5] The central lifeline of RV. [6] Northwestern Rivers:
The gorge is 4,500–5,200 m (14,800–17,100 ft) deep near the Nanga Parbat. The massive amounts of erosion due to the Indus River following the capture and rerouting through that area is thought to bring middle and lower crustal rocks to the surface. [1] Gilgit is the westernmost tributary of the Indus River.
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