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1833 Bihar–Nepal earthquake

Earthquake in Nepal and India

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Geology

The Main Himalayan Thrust is a décollement structure that defines the boundary between the Indian Plate and Eurasian Plate. This thrust fault is the source of most of Nepal's earthquakes. The earthquake of 1833 has been suggested by geologists to be a repeat of the 1344 earthquake, and the 2015 Gorkha earthquake was a repeat of the 1833 event. All of which failed to release all the strain that had been building over the past centuries thus was an incomplete rupture of the Main Himalayan Thrust.

The décollement rupture area of the 1833 event is likely the same as in 2015, but closer to Kathmandu. Both earthquakes occurred along the MHT but did not rupture to the surface, thus, were blind thrust earthquakes. Inferring from isoseismal maps prepared after the quake, researchers believe the earthquake was caused by an 80–120 km × 40 km section of the megathrust rupturing. The same fault patch that ruptured in 1833 would re-rupture again during the Mw 8.0 1934 Bihar earthquake, as the 1833 event did little to release the elastic tension along the décollement.

Very little is known about the epicenter location of the earthquake due to the poor constrains in data. Researcher and seismologist Nicholas Ambraseys determined the epicenter coordinates was 27°42′N 85°42′E / 27.7°N 85.7°E. Another epicenter area located roughly 130 km west of the 1934 earthquake epicenter, at the eastern edge of a seismic gap has been favoured by many authors.

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