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2001 Gujarat earthquake

Earthquake in India and Pakistan

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Through Earthquake, Tehsil and Gujarat

The intraplate earthquake measured 7.6 on the moment magnitude scale and occurred at a depth of 17.4 km (10.8 mi). The earthquake killed at least 20,023 people, injured another 166,000 and destroyed about 400,000 buildings in Gujarat and the Pakistani province of Sindh. The vast majority of deaths and damage were observed in Kutch district, while nearly 1,600 additional deaths occurred in the cities of Ahmedabad, Rajkot, Jamnagar, Surendranagar, Surat, Gandhinagar and Vadodara.

Tectonic setting

Gujarat lies 300–400 km from the plate boundary between the Indian plate and the Eurasian plate, but the current tectonics are still governed by the effects of the continuing continental collision along this boundary. During the break-up of Gondwana in the Jurassic, this area was affected by rifting with a roughly west–east trend. During the collision with Eurasia the area has undergone shortening, involving both reactivation of the original rift faults and development of new low-angle thrust faults. The related folding has formed a series of ranges, particularly in central Kutch.

The focal mechanism of most earthquakes is consistent with reverse faulting on reactivated rift faults. The pattern of uplift and subsidence associated with the 1819 Rann of Kutch earthquake is consistent with reactivation of such a fault.

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