Project Bharatam

Place · shifting river channel · India

The Ganges' eastward migration

Also known as Bhagirathi, Padma, Ganges delta shift, Hooghly decline, The Ganges' eastward migration — Bhagirathi to Padma

Between roughly the sixteenth and eighteenth centuries the main discharge of the Ganges moved from the Bhagirathi–Hooghly in the west to the Padma in the east. Every city that had depended on the western channel was stranded, and the delta's active sedimentation — and its rice frontier — moved into what is now Bangladesh.

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Rivers & waterCatastrophe & landscape
Function
Water & infrastructure
Confidence
Mixed / layered — The channel shift is supported by records and sediment work; its chronology is reconstructed and approximate.
Location
24.200, 88.250 (approximate)

Worth knowing

Gaur, Pandua, Rajmahal, Murshidabad and Tamralipta all decline in the same period and for the same reason. The Farakka barrage, built in 1975 to force water back down the Bhagirathi and keep Calcutta port navigable, is an attempt to reverse this shift by engineering, and is still disputed with Bangladesh.

Caveat.

The chronology of the shift is reconstructed from Mughal revenue records, European maps and sediment work, and the dates are approximate rather than fixed.

Connections (3)

On these journeys

Sources

Wikipedia, “Bhagirathi River”. Richard M. Eaton, The Rise of Islam and the Bengal Frontier 1204–1760 (1993), chapter on the delta's eastward movement; Kanangopal Bagchi, The Ganges Delta (1944).

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