Earthquake risk in Bangladesh The Narsingdi earthquake has shaken us, are we listening?

The Narsingdi earthquake has shaken us, are we listening?

Written by Michael S. Stickler, S. Humayun Akhtar, Ph.D. Mohimanul Islam, Leonardo Sieber, Cecilia McHugh, Abdullah Marouf, Ph.D. Hasnat Juman, and Lin Chen, Ph.D.

Saturday, December 20, 2025 12:00 AM Last updated on: Saturday, December 20, 2025 05:23 PM

Bangladesh is a dynamic land where coal appears and disappears, rivers change, and the coastline grows and erodes over the course of a human lifetime. The Earth is similarly dynamic, but on a much longer time scale. Our planet's solid outer shell is divided into a number of rigid tectonic plates that slowly collide, separate, or slide over each other. Most earthquakes occur at the boundaries between plates. The largest earthquakes occur when two plates move toward each other. These boundaries do not move smoothly; They stumble, build up pressures over hundreds to thousands of years, and then suddenly release that stored motion in a major earthquake. The collision of the Indian plate with Asia led to the formation of the Himalayas and Tibet, and also generated the 2015 Nepal earthquake and the 1950 Assam earthquake. On the eastern side of the Indian plate, the Indian Ocean dips beneath Southeast Asia. The 2004 Sumatra earthquake and tsunami occurred along this border, tearing up a 1,200-kilometre-long area. Another major earthquake struck 500 kilometers from the Arakan coast of Myanmar to Chittagong in 1762.

These plate boundaries continue north into Bangladesh, but the main fault, the megathrust, is buried beneath the sediments of the Ganges-Brahmaputra delta. The Sylhet and Tripura Hills and Chittagong Hills (CHT) are the result of large supra-thrust delta deposits being folded and faulted. The Great Thrust is a very broad, flat interface between the Indian and Burmese plates. It is completely buried by kilometers of sediment and cannot be seen on the surface.

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