A moderate earthquake with a magnitude of 4.3 on the Richter scale struck the Bay of Bengal early Wednesday morning. The National Center for Seismology (NCS) reported that the tremor occurred at 05:12 IST at a depth of 10 kilometers. The epicenter was located at 14.94° N latitude and 90.18° E longitude.

This seismic event follows a similar earthquake of magnitude 4.4 that occurred in the same region in December of last year. While the 4.3 magnitude earthquake is considered moderate, it serves as a reminder of the ongoing seismic activity in this region. Earthquakes of this magnitude can be felt by people and may cause minor damage, but are unlikely to cause widespread destruction.

The Bay of Bengal is a seismically active region, and earthquakes are not uncommon. The region is situated near the collision zone of the Indian and Eurasian tectonic plates, a major driver of seismic activity in the area. The convergence of these plates results in the accumulation of stress in the Earth's crust, which is periodically released in the form of earthquakes.

While this earthquake was relatively moderate, it underscores the importance of continued monitoring and preparedness for seismic events in the region. The NCS and other geological agencies play a crucial role in tracking seismic activity, providing timely information, and assessing potential risks. Their work is essential for informing the public and implementing measures to mitigate the impact of future earthquakes.