Delhi Mild Tremors Felt as 3.2 Magnitude Earthquake Strikes Faridabad
Delhi mild tremors were felt across the National Capital Region on Tuesday morning following a 3.2 magnitude earthquake with its epicenter located in Faridabad. According to the National Centre for Seismology (NCS), the shallow quake, with a depth of just 5 kilometers, was recorded at 6 AM. Fortunately, there have been no immediate reports of any damage to property or loss of life, bringing relief to residents who felt the sudden shaking. This event marks the third earthquake reported in the Delhi-NCR region this month, raising discussions about the area’s seismic activity.
This recent tremor follows two other earthquakes felt in the region earlier in July. On July 10, moderate tremors were experienced after a 4.4 magnitude earthquake with its epicenter in Jhajjar, and just a day later, another quake of 3.7 magnitude struck the same area. Earlier this year, on February 17, a 4.0 magnitude earthquake originating in south Delhi’s Dhaula Kuan also caused mild tremors in the city. These recurring seismic events highlight the region’s susceptibility to tremors, reminding residents of its geological characteristics.
Data from the NCS indicates a history of seismic activity in the Delhi-NCR region. Between 1993 and 2025, the area around Dhaula Kuan alone has recorded 446 earthquakes within a 50 square kilometer radius, with magnitudes ranging from 1.1 to 4.6. This data underscores the high seismic activity in this particular sub-region. The Bureau of Indian Standards classifies the country into four seismic zones, ranging from Zone II (low intensity) to Zone V (very severe). Delhi and the NCR fall under Zone IV, categorized as a “severe” seismic zone, which makes seismic occurrences relatively frequent in this densely populated area.
Experts have pointed out that Delhi’s vulnerability is further compounded by the presence of three active fault lines—the Sohna, Mathura, and Delhi-Moradabad faults—that run directly through the city. Neighboring Haryana also has a higher number of such fault lines, with seven identified. Additionally, the capital’s geographical proximity to the seismically active Himalayan region increases the likelihood of experiencing tremors, including potential aftershocks from larger events in that area. City authorities and disaster management teams maintain preparedness protocols for such occurrences.
This series of tremors serves as a regular reminder for Delhi and the NCR of their location in a seismically active zone. While Tuesday’s earthquake was mild with no reported damage, the ongoing activity emphasizes the importance of adherence to earthquake-resistant building codes and continued public awareness regarding safety measures for all residents.
