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Geography of Mizoram

Geography of the Indian state of Mizoram

  • 4 min read
  • 8 chapters

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Mizoram’s terrain is shaped by the collision of the Indian and Burmese tectonic plates, resulting in a folded, north-south hill system with perpendicular faults. The state lies in India’s highest seismic zone (Zone VI), experiencing frequent earthquakes. Notable events include a 4.3 magnitude quake near Kolasib on 19 April 2011 and a 6.4 magnitude quake on 4 February 2011. More recently, a 5.2 magnitude earthquake struck Champhai district on 12 January 2025, highlighting ongoing seismic activity. The geological structure comprises sedimentary rocks from the Surma (Middle Bhuban Formation), Barail, and Tipam groups, with alluvium in riverbeds containing argillaceous and arenaceous sandstones, shale, siltstones, mudstones, and greywacke. A 560 m thick Middle Bhuban rock succession between Bawngkawn and Durtlang, showing seven normal and seven reverse magneto-strata, dates to approximately 20 million years old. These rocks are weak, weathered, and prone to landslides, especially during monsoons, due to high slopes and seismic activity. Locally, soft black-to-grey rock is used for building materials and low-traffic roads. Soils are typically sandy loam and clay loam, heavily leached, porous, and low in minerals and humus. No economically significant minerals are present, though clay, sand, and gravel deposits occur in riverbeds like the Tlawng. Mizoram’s geological conditions have spurred oil and gas exploration, with international companies from France, Russia, and Cyprus signing agreements in 2009 for a 12% oil and 10% gas royalty to the state, though no major reserves have been confirmed as of 2025.

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