Islamabad: Pakistan woke as much as a jolt early Friday morning as an earthquake of magnitude 5.2 struck the nation, in accordance with the Nationwide Centre for Seismology (NCS). The earthquake occurred at a depth of 135 kilometres, sending tremors throughout a number of areas.
The NCS shared the technical particulars of the quake on X, stating, “EQ of M: 5.2, On: 21/11/2025 03:09:12 IST, Lat: 36.12 N, Lengthy: 71.51 E, Depth: 135 Km, Location: Pakistan.”
Authorities are monitoring the state of affairs, and extra data on damages or casualties is anticipated.
Seismologists clarify that shallow earthquakes are usually extra harmful than deeper ones as a result of the seismic waves attain the floor shortly, producing stronger floor shaking. This could improve injury to buildings and lift the chance of accidents or fatalities.
The area encompassing Afghanistan, Pakistan and northern India is among the most seismically lively zones on the planet. It sits on the collision boundary of the Indian and Eurasian tectonic plates, making it susceptible to average and powerful earthquakes that may be felt throughout nationwide borders.
Pakistan, specifically, lies on a number of main fault traces and is taken into account one of many world’s most earthquake-prone international locations. Provinces like Balochistan, Khyber Pakhtunkhwa and Gilgit-Baltistan sit on the southern fringe of the Eurasian plate, whereas Punjab and Sindh lie on the northwestern fringe of the Indian plate, making a excessive danger of frequent seismic occasions.
Balochistan is particularly susceptible as a result of it sits close to the lively boundary between the Arabian and Eurasian plates. Punjab additionally experiences periodic tremors attributable to its tectonic location, and whereas Sindh is barely much less in danger, it stays inclined to seismic exercise due to its positioning alongside the plate edges.
Authorities proceed to observe the aftershocks and are urging residents within the affected areas to stay alert and observe security protocols.

