Significant earthquakes of 2013

November 28, 2013 Earthquake: Borazjan, Iran

November 28, 2013 · M5.8 · 8 deaths · 250 houses destroyed

A magnitude 5.8 earthquake struck Borazjan, Iran on November 28, 2013 at 13:51:34 UTC, 8 km below the surface. It killed 8 people.

Map

Where it struck, with the other significant earthquakes within 200 km. Circles are sized and colored by magnitude; select one for its page.

The earthquake

Date
November 28, 2013
Time
13:51:34 UTC
Place
Borazjan, Iran
Magnitude
5.8 (Mw)
Focal depth
8 km (5 mi)
Intensity
5 on the Modified Mercalli scale
Tsunami
None recorded
Epicenter
29.320° N, 51.310° E
Country
Iran

The toll

Deaths
8
Injuries
200
Damage
Moderate (about $1 to $5 million)
Houses destroyed
250
Houses damaged
Few (about 1 to 50)

Where the literature gives no number, NCEI records a description on a scale of 1 to 4, printed here in its words. Damage is in millions of US dollars of the year of the event, not adjusted for inflation.

What the record says

NCEI’s account, from the sources it cites.

Eight people killed, at least 200 injured, buildings damaged and electricity disrupted in the Borazjan area. Felt (IV) at Bandar-e Bushehr. Also felt at Bandar-e Ganaveh. Felt at Al Budayyi', Bahrain and at Ad Dasmah, Ad Dawhah, Kuwait City and Salwa, Kuwait.

Tectonic Summary

Seismotectonics of the Middle East and Vicinity

No fewer than four major tectonic plates (Arabia, Eurasia, India, and Africa) and one smaller tectonic block (Anatolia) are responsible for seismicity and tectonics in the Middle East and surrounding region. Geologic development of the region is a consequence of a number of first-order plate tectonic processes that include subduction, large-scale transform faulting, compressional mountain building and crustal extension...

Off the south coast of Pakistan and southeast coast of Iran, the Makran trench is the present-day surface expression of active subduction of the Arabia plate beneath the continental Eurasia plate, which converge at a rate of approximately 20 mm/yr. Although the Makran subduction zone has a relatively slow convergence rate, it has produced large devastating earthquakes and tsunamis. For example, the November 27, 1945 M8.0 mega-thrust earthquake produced a tsunami within the Gulf of Oman and Arabia Sea, killing over 4,000 people. Northwest of this active subduction zone, collision of the Arabia and Eurasia plates forms the approximately 1,500-km-long fold and thrust belt of the Zagros Mountains, which crosses the whole of western Iran and extends into northeastern Iraq. Collision of the Arabia and Eurasia plates also causes crustal shortening in the Alborz Mountains and Kopet Dag in northern Iran. Eastern Iran experiences destructive earthquakes that originate on both strike-slip and reverse faults. For example, the 16 September 1978 M7.8 earthquake, along the southwest edge of the Dasht-e-Lut Basin killed at least 15,000 people.

(above from reference #13456)

Tehran (AFP) - A 5.7 magnitude earthquake on the Gulf coast near Iran's sole nuclear power plant killed eight people and injured 190 on Thursday, emergency response chief Hassan Qadami told state media. "So far, there are seven dead and 30 injured receiving hospital treatment," the official IRNA news agency quoted Qadami as saying. However, an official said the temblor had "not created any problem for the activities of the power plant" at Bushehr, where Iran has its Russian-built reactor. The quake's epicentre was near Borazjan, around 60 kilometres (35 miles) from Bushehr. The media said the quake had destroyed around 250 homes and businesses, while Dashtestan provincial Governor Alireza Khorani also spoke of damaged houses and electricity pylons. (reference #10815)

Other significant earthquakes nearby

Within 200 km, the deadliest first.

More

Significant earthquakes of 2013The 2000sEvery quake the USGS located in 2013Recent earthquakes near hereThis day in weather history

Sources

Significant earthquakes from NOAA’s National Centers for Environmental Information, Global Historical Hazard Database, cited as NCEI/WDS, doi:10.7289/V5PN93H7. Public domain. Read 2026-09-24. NCEI earthquake 10056.