Mapping of palaeochannels using multi sensor remote sensing data from WIFS, MSS-I, LISS-III and PAN sensors from Indian remote Sensing Satellites IRS 1B and ID was carried out using digital image processing techniques. The Ancient Indus Valley:New perspectives, http://www.pnas.org/content/109/26/E1688.abstract, http://www.jatland.com/w/index.php?title=Chautang_River&oldid=350630. It then turns west at Kedara and also flows underground. Haryana which lies on the Chautang River was the site of an extensive city, part of the Indus Valley Civilization. Subsquently, Keith (1922) and Dey (1927) also supported the course of the Drishadvati as being the present Chautang river and then along the Hansi —Hissar branch of the western Yamuna canal. The literary tradition represented in the main by the faithfully preserved corpus of Vedic texts headed by the Rigveda. [2] However, as per recent studies Yamuna changed its course towards East some 50,000 to 10,000 years ago and Chautang is a rain-fed river and Yamuna is not pouring any water into it from last 10,000 years. — (Rigveda – 2. The river is known as Ghaggar before the Ottu barrage and as the Hakra downstream of the barrage. Yamuna (Somb, Thapana, Sahibi) Hathini Kund Barrage, Yamuna Nagar has virtually deprived the river of environmental flow, hence the river for its entire length ~200 km upstream Delhi is turned seasonal. 16), Sarasvati and Drishadvati: The Archaeological Findings, Sarasvati and Drishadvati: Scientific Research, Ancient Sarasvati and present Ghaggar-Hakra System: Relation, Sarasvati and Drishadvati: In recent NEWS, Rajasthan Government Announces Diwali 2020 Bonus for Employees, UGC Issues Guidelines for Re-opening of Colleges & Universities, Ministry of Culture issues SOPs for Re-opening of Museums Art Galleries Exhibitions, Rajasthan Sujas September October 2020 Download PDF, Second Wave of Covid-19 in Rajasthan Expected Mid-December 2020, Privacy Policy | Terms of Use | Disclaimer. Supposed position east of the Indus, which corresponds with the Ghaggar-Hakra riverbed. The drainage pattern for all these rivers is dendritic. Drilling work at fourteen locations in Dharmikhu – Kuriaberi – Ghantiyali – Ranau Longewala – Ghotaru sections, and the radiocarbon age analysis of the water samples thus obtained. [3] However, according to Giosan, the Chautang is a rain-fed river, and the Yamuna changed its course towards east some 50,000 to 10,000 years ago, and didn't pour any water into it for the last 10,000 years. The Lost Rivers of Rajasthan: Scientific Research Saravati River. [3] However, according to Giosan, the Chautang is a rain-fed river, and the Yamuna changed its course towards east some 50,000 to 10,000 years ago, and didn't pour any water into it for the last 10,000 years.