All you need to know about 1897 Earthquake in Meghalaya & Assam

All you need to know about 1897 Earthquake in Meghalaya & Assam

TNT Desk | April 30, 2018

June 12, 1897 has been recorded in the history of Meghalaya and Assam as one of the most horrific day as the day is marked with the most powerful earthquake recorded in human history. This earthquake was 50 times more powerful than the tremor that hit San Fransisco. It may be mentioned that since Meghalaya attained its statehood on January 21, 1972, the earthquake is normally referred to as having occurred in Assam as Meghalaya was still a part of Assam then.

The Assam earthquake of 1897 occurred on 12 June in Assam at 17:15 local time, India, and had an estimated moment magnitude of 8.0. Considering the size of the earthquake, the mortality rate was not that high, with about 1,542 casualties, but property damage was very heavy. Damage from the earthquake extended into Calcutta where dozens of buildings were badly damaged or partially collapsed. Shaking from the event was felt across India, as far as Ahmedabad and Peshawar. Seiches were also observed in Burma.


The earthquake occurred on the SSW-dipping reverse Oldham fault that forms the northern edge of the Shillong Plateau within the Indian Plate. There was a minimum displacement on the main fault of 11 m, although up to 16 m has been calculated, one of the greatest for any measured earthquake. The calculated area of slip extended 180 km along strike and from 9–45 km below the surface, indicating that the entire thickness of the crust was involved.

Thought to have happened 32 km underground, the earthquake left masonry buildings in ruins over 400,000 km2 area and was felt over 650,000 km2 from Burma to Delhi. Numerous buildings in the neighboring country of Bhutan were heavily damaged. Dozens of aftershocks were felt in and around the region with the last event being felt on 9 October 1897 at 01:40 UT in Calcutta.

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The earthquake resulted in Shillong Plateau being thrust violently upwards by about 11 metres. The fault was about 110 km in length while the fault slip was about 18 m (accuracy more or less by 7 m). At the epicentre, vertical acceleration is thought to have been above 1g force and surface velocity 3 m/s.

In Shillong, the earthquake damaged every stone house and half the houses built of wood. The shock levelled the ground and resulted in 13 deaths. Fissure were also reported in the area. In Cherrapunji, it resulted in a landslide, which led to 600 deaths. In Goalpara, it resulted in waves from the river Brahmaputra, on which bank the town is situated, destroying the market. In Nalbari, there were reported sightings of earth-waves and water waves. In Guwahati, the earthquake lasted for 3 minutes. the Brahmaputra river rose by 7.6 ft. Damage were caused to Umananda Island temple and railway lines. 5 people died. In Nagaon, every brick house was damaged, while traditional houses made of wood, with grass roofs were bent. There were many small fissures/volcanos and the road were impassable for vehicles.

There were hundreds of aftershocks—some very heavy and some light at Shillong, Tura, Bijni, Guwahati and other nearby areas. At Bordwar tea estate, a week after the great shock, the surface of a glass of water standing on a table was in a constant state of tremor. At Tura, a hanging lamp was kept constantly on the swing for 3 days. According to reports in the Assam newspaper, in North Guwahati there were 561 aftershocks till the end of the 15th of June, 125 between 15th to 30th June, and 84 from 1st to 15th July. Most of the aftershocks were local and not felt over a large area.



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