Minor 3.0-Magnitude Tremor Shakes Central Bangladesh Near Narsingdi

A mild earthquake registering a magnitude of 3.0 on the Richter scale struck central parts of Bangladesh in the early hours of Monday, causing brief tremors across the region without resulting in any reported casualties or material damage.

The seismic event occurred precisely at 5:32 AM local time, according to an official bulletin issued by the Bangladesh Meteorological Department (BMD). Scientists at the BMD’s Seismic Observatory identified the epicentre in the Shibpur sub-district, located within the Narsingdi district. The focal point of the earthquake was positioned approximately 47 kilometres north-east of Dhaka, with an estimated hypocentral depth of 10 kilometres beneath the terrestrial surface.

Summary of Event Parameters

• Date & Local Time: Monday, 5:32 AM (BST)

• Richter Magnitude: 3.0 (Minor classification)

• Geographical Epicentre: Shibpur Upazila, Narsingdi

• Distance to Capital: 47 km North-East of Dhaka

• Hypocentral Depth: 10 km

• Casualties & Loss: Zero reported

Because the focal depth was relatively shallow, minor vibrations were discernible to early morning residents across Narsingdi and adjacent areas of the Greater Dhaka region. However, due to the limited energy release associated with a magnitude 3.0 quake, emergency services confirmed that municipal infrastructure, residential structures, and public utility networks remained completely unaffected.

Geologically, Bangladesh sits at the junction of three major colliding tectonic plates: the Indian, Eurasian, and Burmese plates. This geographical position renders several zones across the country—particularly the northern, north-eastern, and central fault bands like the Dauki Fault and the Madhupur Fault zone—susceptible to tectonic stresses. Geoscientists note that minor intraplate events of this nature occur periodically in the central plains. Whilst a magnitude 3.0 tremor is generally harmless, such events reinforce the necessity for ongoing seismic surveillance and adherence to structural building codes throughout the region. Meteorological officials confirmed that monitoring systems remain active and no immediate aftershocks were detected.