A 2.8 magnitude earthquake shook New Delhi on Monday morning, causing brief tremors in parts of the national capital. The National Centre for Seismology reported that the earthquake occurred at around 8:44 a.m. with its epicenter in North Delhi at a shallow depth of 5 kilometers.
Fortunately, there were no immediate reports of casualties or property damage, and the tremors were described as mild. This event once again emphasized Delhi’s susceptibility to seismic activity due to its geological location.
Delhi and the surrounding National Capital Region (NCR) are close to active fault lines, making the area prone to frequent low- to moderate-intensity earthquakes. Experts caution that even mild tremors should not be disregarded as they highlight the seismic risks faced by the densely populated capital.
Geological conditions, especially in the eastern parts of Delhi along the Yamuna floodplains, further increase the risk. These areas have soft, sandy, and silty soil with groundwater close to the surface, which can amplify seismic waves during an earthquake, potentially leading to structural damage.
India’s seismic zoning system was updated in 2025, with Delhi remaining in Zone IV, indicating a high-risk region. Neighboring cities in Uttar Pradesh, such as Bulandshahr, Deoria, Ghaziabad, Gorakhpur, Moradabad, and Pilibhit, are also classified under Zone IV, underscoring the seismic vulnerability of northern India.
In November 2025, a stronger earthquake measuring 5.7 hit Bangladesh’s Narsingdi district, with tremors felt in parts of eastern India, including Kolkata, showcasing the interconnected seismic activity in the region.
