The 6.4 Mw Zarand earthquake shakes the Kerman Province of Iran with a maximum Mercalli intensity of VIII (Severe), leaving 612 people dead and 1,411 injured.

The 2005 Zarand Earthquake: A Morning of Devastation in Kerman Province

In the quiet dawn of February 22, 2005, at precisely 05:55:23 local time, a powerful earthquake shattered the tranquility of Iran's southeastern Kerman province. This significant natural disaster brought widespread destruction, particularly to several villages surrounding the city of Zarand, leaving an indelible mark on the landscape and its communities. The seismic event unfolded in a region known for its geological activity, catching many residents unprepared as the ground began to tremble with immense force.

Seismic Magnitude and Geographic Context

Measuring 6.4 on the moment magnitude scale, the Zarand earthquake was a potent demonstration of the Earth's raw power. Such a magnitude indicates a substantial release of energy from the planet's crust. The intensity of the ground shaking was equally severe, registering a maximum Mercalli intensity of VIII. This classification signifies a 'Severe' impact, capable of causing considerable damage to well-built structures and leading to general alarm among the populace. The affected city of Zarand itself is situated approximately 740 kilometers southeast of Iran's bustling capital, Tehran, placing it in a distinct geological zone.

The Devastating Human Cost and Recorded Impact

The aftermath of the 2005 earthquake quickly revealed a tragic human toll. According to comprehensive reports from both the United States' National Earthquake Information Center and the Belgian Centre for Research on the Epidemiology of Disasters, the catastrophic event resulted in 612 fatalities and left 1,411 people injured. These figures underscore the profound impact on local communities. Beyond the human suffering, the earthquake's mechanical force was also meticulously recorded; at the Shirinrud dam, for instance, a maximum peak ground acceleration of 0.51 g was observed. This specific measurement provides a scientific glimpse into the intense ground motion experienced during one of Iran's most impactful recent seismic events.