North Delhi was jolted by a magnitude 2.9 earthquake in the early hours of Sunday, August 2, 2026, the National Center for Seismology said.
The quake struck at 4:14 am IST, with its epicenter located at 28.721 degrees North and 76.957 degrees East, at a depth of 8 kilometres.
Residents reported feeling brief tremors, with some stepping outside as a precaution, though no injuries or property damage have been reported.
The National Center for Seismology confirmed the earthquake’s magnitude, timing, depth and epicenter using its official seismic monitoring network.
The National Capital Region lies within Seismic Zone-4, a designation tied to its exposure to recurring mild earthquakes caused by active fault lines.
No advisory has been issued by authorities so far, in line with the standard response to low-magnitude quakes that cause no structural damage.
Experts have repeatedly noted that Delhi-NCR experiences periodic mild tremors because of this fault activity, though most such events, including Sunday’s, are too weak to cause structural damage.
Authorities did not issue any advisory or alert following the tremor, consistent with standard practice for earthquakes below magnitude 4 that cause no reported damage.
Delhi has recorded several similar minor tremors in recent years, most of them below magnitude 4, with seismologists attributing the frequency to the Delhi-Haridwar ridge and other fault systems running beneath the National Capital Region.
The National Center for Seismology operates a nationwide network of seismographic stations that continuously monitor ground movement, allowing it to detect and report even minor tremors like Sunday’s within minutes of occurrence.
The National Center for Seismology confirmed the tremor’s parameters shortly after it occurred, as it does for all seismic events detected across the country’s monitoring network.
Delhi and the wider National Capital Region fall within Seismic Zone-4 on India’s seismic hazard map, a classification that denotes high vulnerability to earthquakes due to active fault lines running beneath the region.
Photo by Frederick Noronha, Wikimedia Commons, CC BY-SA 4.0
