Historedia
Asia PacificEvent

Rann of Kutch earthquake

When
1819
Where
Rann of Kutch
Episodes
3

The 1819 Rann of Kutch earthquake occurred on 16 June 1819, with an estimated magnitude of 7.7 to 8.2. It triggered a tsunami, caused at least 1,543 deaths, and transformed the Nara river delta into a marshy wasteland. Prolonged aftershocks continued for decades, potentially influencing later seismic events.

Episodes

  1. 1819–1869 · Rann of KutchProlonged Aftershock Activity

    Major earthquakes continued for at least 50 years following the main shock, including one in 1846.

  2. 1819–2001 · Rann of KutchStress Transfer Implications

    Coulomb stress transfer from the 1819 earthquake may have triggered the 2001 Bhuj earthquake.

  3. 16 June 1819 · Rann of Kutch1819 Rann of Kutch Earthquake

    The earthquake occurred on 16 June 1819, causing at least 1,543 deaths and transforming the Nara delta.

Background and detail

Background. Before 1819, the Nara was a massive, active freshwater branch of the Indus. The 1819 earthquake is described as having transformed this complex, organized river delta into the chaotic, marshy wasteland of creeks and salt lakes seen today. The 1956 Anjar earthquake was due to reverse faulting similar in type to that which is thought to have caused the 1819 Rann of Kutch earthquake.

Impact. The earthquake had an estimated magnitude ranging from 7.7 to 8.2 and a maximum perceived intensity of XI. It triggered a tsunami and caused at least 1,543 deaths. The main shock was followed by prolonged aftershock activity, with major earthquakes continuing for at least 50 years, including one in 1846.

Sources

  1. 1819 Rann of Kutch earthquake Wikipedia, revision of 2026-07-26

Machine-drafted from the cited Wikipedia passages and checked by a reviewing model, not by a human editor. Every passage cites the revision it was written from; dates and places follow those passages.