Indus Valley Civilisation sites

3300 – 1300

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dubna 10, 2026

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"Scholars such as Romila Thapar, Irfan Habib and the late RS Sharma started questioning this identification in the 1980s. What prompted this rather late reaction? It was a new development: A study of the evolution of the pattern of Harappan settlements in the Saraswati basin now revealed that in its central part — roughly southwest Haryana, southern Punjab and northern Rajasthan — most or all Harappan sites were abandoned sometime around 1900 BCE, a period coinciding with the end of the urban phase of the Indus civilisation. Clearly, the river system collapsed — which archaeologists now saw as a factor contributing to the end of the brilliant Indus civilisation. Why was this a problem? We must remember that the Saraswati is lavishly praised both as a river and a Goddess in the Rig Veda, a collection of hymns which mainstream Indology says was composed by Indo-Aryans shortly after their migration to India around 1500 BCE. However, by that time, the Saraswati had been reduced to a minor seasonal stream: How could the said Aryans praise it as a ‘mighty river’, the ‘best of rivers’, ‘mother of waters’, etc? There is a chronological impossibility. Hence, the objectors asserted, the Ghaggar-Hakra was not, after all, the Saraswati extolled in the Rig Veda. While some (Rajesh Kochhar) tried to relocate the river in Afghanistan, others (Irfan Habib) decided that the Saraswati was not a particular river but “the river in the abstract, the River Goddess”; but both theses ran against the Rig Veda’s own testimony that the river flowed between the Yamuna and the Sutlej."

- Indus Valley Civilisation sites

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"In contrast, changes taking place in the Saraswati Valley in the early second millennium were probably a major contributor to the Indus decline. In Harappan times, the Saraswati was a major river system flowing from the Siwaliks at least to Bahawalpur, where it probably ended in a substantial inland delta. The ancient Saraswati River was fed by a series of small rivers that rose in the Siwaliks, but it drew the greater part of its waters from two much larger rivers rising high in the Himalayas: the Sutlej and the Yamuna. In its heyday the Saraswati appears to have supported the densest settlement and provided the greatest arable yields of any part of the Indus realms. The Yamuna, which supplied most of the water flowing in the Drishadvati, a major tributary of the Saraswati, changed its course, probably early in the second millennium, to flow into the Ganges drainage. The remaining flow in the Drishadvati became small and seasonal: Late Harappan sites in Bahawalpur are concentrated in the portion of the Sarawati east of Yazman, which was fed by the Sutlej. At a later date the Sutlej also changed its course and was captured by the Indus. These changes brought about massive depopulation of the Saraswati Valley, which by the end of the millennium was described as a place of potsherds and ruin mounds whose inhabitants had gone away. At the same time new settlements appeared in the regions to the south and east, in the upper Ganges-Yamuna doab. Some were located on the palaeochannels that mark the eastward shift of the Yamuna. Presumably many of the Late Harappan settlers had originated in the Saraswati Valley."

- Indus Valley Civilisation sites

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