An earthquake of magnitude 4.3 rocked Afghanistan on Saturday, a press release by the Nationwide Centre for Seismology (NCS) mentioned. As per the NCS, the earthquake occurred at a shallow depth of 15 km, making it prone to aftershocks.
In a submit on X, the NCS mentioned, “EQ of M: 4.3, On: 03/05/2025 13:20:36 IST, Lat: 36.52 N, Lengthy: 71.20 E, Depth: 15 Km, Location: Afghanistan.”
Shallow earthquakes are extra harmful than deeper ones attributable to their larger power launch nearer to the Earth’s floor, inflicting stronger floor shaking and elevated harm to constructions and casualties, in comparison with deeper earthquakes, which lose power as they journey to the floor.
On Friday, an earthquake of magnitude 4.5 on the Richter Scale jolted Afghanistan, a press release by the Nationwide Centre for Seismology (NCS) mentioned. As per the NCS, the earthquake occurred at a depth of 150km.
In a submit on X, NCS mentioned, “EQ of M: 4.5, On: 02/05/2025 20:20:58 IST, Lat: 35.00 N, Lengthy: 68.27 E, Depth: 150 Km, Location: Afghanistan.”
As per the United Nations Workplace for the Coordination of Humanitarian Affairs (UNOCHA), Afghanistan stays extremely susceptible to pure disasters, together with seasonal flooding, landslides and earthquakes.
These frequent earthquakes in Afghanistan trigger harm to susceptible communities, that are already grappling with a long time of battle and under-development and have left them with little resilience to deal with a number of simultaneous shocks, UNOCHA famous.
Afghanistan has a historical past of highly effective earthquakes, and the Hindu Kush Mountain vary is a geologically lively space the place quakes happen yearly, based on the Crimson Cross. Afghanistan sits on quite a few fault traces between the Indian and the Eurasian tectonic plates, with a fault line additionally working immediately by means of Herat. Its location on a number of lively fault traces alongside the collision zone between the Indian and Eurasian tectonic plates makes it a seismically lively area. These plates meet and collide, inflicting frequent seismic exercise.
