Iran is situated at the convergence of several tectonic plates, including the Arabian, Eurasian, and Indian plates. This geological setting results in significant seismic activity, with approximately 273 earthquakes of magnitude 4 or above occurring annually within 300 km of Iran. Since 1950, around 172,300 people have died due to earthquakes in the country.

Iran's earthquake history is marked by numerous significant seismic events that have shaped its society and infrastructure. Continuous monitoring and research are essential to improve earthquake prediction and preparedness in this seismically active region.