"Provisional age data now show that between 2000 and 3000 BCE, flow along a presently dried-up course known as the Ghaggur-Hakkra River ceased, probably driven by the weakening monsoon and possibly also because of headwater capture into the adjacent Yamuna and Sutlej Rivers."
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Academics from the United KingdomUniversity of Oxford alumniGeologists from EnglandUniversity College London facultyUniversity of Edinburgh alumni
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Peter Clift
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