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Rann of Kutch

Large area of salt desert in India and Pakistan

  • 4 min read
  • 6 chapters

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Through Indian subcontinent, Gujarat and Tectonics

Origin and formation

In the Mesozoic era (252 to 66 mya), the area was a low lying peneplain, covered by shallow waters of the Arabian Sea. It became part of a large inland lake when the connection to the sea was cut off after land upliftment due to tectonic movement. When the waters recede in the dry season, it left behind the seasonal salt marshes, which formed the Rann of Kutch.

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