Jane McIntosh

Jane McIntosh is a Scottish archaeologist and author.

Quotes

• The Indus civilization has challenged scholars’ understanding since its discovery some eighty years ago, and in recent years the application of systematic and problem-orientated research, coupled with much new and unexpected data, has overturned many previous interpretations.
  • Jane McIntosh, The Ancient Indus Valley, 2008

• 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.
  • Jane McIntosh, The Ancient Indus Valley, 2008

• The decline of Harappan urbanism probably had many contributing factors. The shift to a concentration on kharif cultivation in the outer regions of the state may have seriously disrupted established schedules for craft production, civic flood defense, building and drain maintenance, and other publicly organized works on which the smooth running of the state depended. The reduction in the waters of the Saraswati and the response of its farmers by migrating into regions to the east tore apart the previous unity of the Harappan state, disrupting its cohesion and its ability to control the internal distribution network.
  • Jane McIntosh, The Ancient Indus Valley, 2008

• ‘[The desertion of the Drishadvati and the Sutlej] is typical of the instability of the river courses in the Indus plains—but in the case of the Saraswati, the effect was not localized but devastating on a major scale. Cities, towns, and villages were abandoned, their inhabitants drifting to other regions of the Indus realms and eastward towards the Ganges, pushing back the centuries-old eastern boundaries of Indus culture and venturing into uncharted territory.’
  • McIntosh, Jane R., A Peaceful Realm°, p. 190.in Danino, M. (2010). The lost river : on the trail of the Sarasvatī. Penguin Books India.

• This work revealed an incredibly dense concentration of sites, along the dried-up course of a river that could be identified as the ‘Saraswati’. . . Suddenly it became apparent that the ‘Indus’ Civilization was a misnomer—although the Indus had played a major role in the rise and development of the civilization, the ‘lost Saraswati’ River, judging by the density of settlement along its banks, had contributed an equal or greater part to its prosperity...Many people today refer to this Early state as the ‘Indus-Saraswati Civilization’ and continuing references [in her book] to the ‘Indus Civilization’ should be seen as an abbreviation in which the ‘Saraswati’ is implied.
  • McIntosh, Jane R., A Peaceful Realm°, p. 24. in Danino, M. (2010). The lost river : on the trail of the Sarasvatī. Penguin Books India.

• The now-dry Hakra River forms part of this river system. Surveys along its dry bed revealed that this was one of the most densely populated areas of the 3rd millennium, the agricultural heartland of the civilization, although it is now virtually desert.
  • McIntosh, Jane R., A Peaceful Realm . quoted in A Reply to Michael Witzel’s ‘Ein Fremdling im Rgveda’ (Journal of Indo-European Studies, Vol. 31, No.1-2: pp.107-185, 2003) by Vishal Agarwal 11 August 2003

• In the Indus period the Saraswati river system may have been even more productive than that of the Indus, judging by the density of settlement along its course. In the Bahawalpur region, in the western portion of the river, settlement density far exceeded that elsewhere in the Indus civilization . . . While there are some fifty sites known along the Indus, the Saraswati has almost a thousand . . . [The Yamuna] shifted its course eastward early in the second millennium, eventually reaching its current bed by the first millennium, while the Drishadvati bed retained only a small seasonal flow; this seriously decreased the volume of water carried by the Saraswati. The Sutlej gradually shifted its channel northward, eventually being captured by the Indus drainage . . . The loss of the Sutlej waters caused the Saraswati to be reduced to the series of small seasonal rivers familiar today. Surveys show a major reduction in the number and size of settlements in the Saraswati region during the second millennium.
  • McIntosh, Jane R., The Ancient Indus Valley: New Perspectives°, pp. 20-21.in Danino, M. (2010). The lost river : on the trail of the Sarasvatī. Penguin Books India.

• 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.
  • Jane McIntosh, The Ancient Indus Valley, 2008