2012 East Azerbaijan earthquakes

2012 East Azerbaijan earthquakes
Date August 11, 2012
Origin time 16:53:17 (UTC+04.30) (mainshock)
17:04:35 (UTC+04.30) (aftershock)
Magnitude 6.4 Mw,[1] 6.3 Mw[1]
Depth 9 km (5.6 mi)
Epicenter 38°19′19.2″N 46°52′48″E / 38.322000°N 46.88000°ECoordinates: 38°19′19.2″N 46°52′48″E / 38.322000°N 46.88000°E
Areas affected Iran
Max. intensity VII – VIII
Aftershocks at least 60 [2][3]
Casualties 306 dead, 3,037 injured [4]

The 2012 East Azerbaijan earthquakes occurred near the cities of Ahar and Varzaqan in Iran's East Azerbaijan Province, on August 11, 2012, at 16:53 Iran Standard Time. The two quakes measured 6.4 and 6.3 on the moment magnitude scale, and were separated by eleven minutes. The epicenter of the earthquakes was 60 kilometers (37 miles) from Tabriz.[5] At least 306 people died and more than 3000 others were injured,[4] primarily in the rural and mountainous areas to the northeast of Tabriz (though 45 died in the city of Ahar).[6] The earthquake was felt in Armenia and Azerbaijan, though no major damage was reported.[7]

Iran is prone to frequent severe earthquakes because several major fault lines cross the country. Earthquakes in 2003 and 1990 killed approximately 26,000 and 40–50,000 people, respectively.

Tectonic setting

Iran lies within the complex zone of continental collision between the Arabian Plate and the Eurasian Plate, which extends from the Bitlis-Zagros belt in the south to the Greater Caucasus mountains, the Absheron-Balkan Sill and the Kopet Dag mountains in the north.[8] The collision between these plates deforms an area of ~ 3,000,000 km2 of continental crust. It is one of the largest convergent deformation regions on Earth.[9] In northwestern Iran, the Arabian Plate is moving northwards at about 20 mm per year relative to the Eurasian Plate, somewhat oblique to the plate boundary zone. The deformation in the area near Tabriz is dominated by the North Tabriz Fault, a WNW-ESE trending right-lateral strike-slip fault, which has been responsible for 7 historical earthquakes of magnitude greater than 6 since AD 858.[10] Other known active faults include a W-E trending fault between the cities of Ahar and Heris.[11]

Earthquakes

USGS ShakeMap for the mainshock

The 6.4 and 6.3 intraplate earthquakes occurred as a result of oblique strike-slip faulting in the shallow crust about 300 km east of the Eurasia-Arabian Plate boundary. The two earthquakes are separated by 10 km in an east-west direction.[12]

Damage and casualties

Iran's state television reported the quake hit near the towns of Ahar, Heris and Varzaqan in East Azerbaijan Province at 4:53 p.m. local time (12:23 GMT). "268 people, 219 women and 49 men, lost their lives in hospitals" while the rest were killed on the spot, Iran's Health Minister Marzieh Vahid-Dastjerdi said. The Iranian minister added that 3,037 people have been injured as a result of Saturday's temblors. According to the head of Iran's Rescue and Relief Organisation, access to villages has been cut and the only communication is via radio. The worst damage and most casualties were in villages near the towns of Ahar, Varzaghan and Heris.[13] In villages near Varzaqan, with most men away from home working, the many mud brick houses which collapsed trapped mainly women and children inside.[14]

Many villages were completely destroyed

Sixty-six rescue teams were sent to the affected region, along with about 200 ambulances and five helicopters. 130 villages were 70-90% destroyed, and 20 were completely leveled. At least 45 people died and more than 500 were injured in Ahar, where electricity and phone lines were cut after the quakes.[3][15][16] More than 40 people died in the city of Varzaqan and 50 were killed in Heris.[2][17] The medical infrastructure in the catastrophe stricken region is not sufficient, and many heavily injured did not survive the rather long way to the nearest hospital.[18]

Most parts of Tabriz also lost electricity, and the city had a large traffic jam. Some buildings were structurally damaged.[6] Over 200 people in Varzaqan and Ahar were extricated from under the debris of collapsed buildings, and local provincial officials asked people in the region to stay outdoors during the night because of the danger of aftershocks. Some residents needed bread, tents and drinking water.[19]

Population exposure from the first shock
Population exposure from the second shock

Rescue teams continued searching for survivors through the night, Iranian officials said they expected the death toll to rise. Between ten and twenty villages close to the epicenter were still cut off from aid and it would take some time to reach them. The Iranian government estimated at least 16,000 people spent the first night after the quakes in emergency shelters.[3]

A day after the quakes, more than 36,000 people had been given emergency shelter, and the Iranian government had dispatched nearly 100 ambulances, 1,100 Red Crescent workers, 44,000 food packages and 5,600 tents. According to Red Crescent officials, more than 1,000 villages were affected by the disaster, and at least 5,000 people were injured. Hospitals in the region's major cities were overcrowded and struggling to cope with the large number of people waiting for treatment.[20]

Aftershocks

Since the main earthquake hit northeast of Tabriz, at least 80 aftershocks have been felt. The strongest measured 6.3 on the moment magnitude scale and occurred eleven minutes after the initial 6.4 quake. A 5.0 quake struck three hours later and, early on August 12, a 5.1 aftershock struck 31 km southwest of Ahar.[21][22]

On August 14, three days after the initial quakes, another 5.1 aftershock struck the same area at a depth of 10 km.[21] An even stronger 5.3 tremor occurred on August 15, approximately 34 km southwest of Ahar.[23]

Reaction

A relief car of Iranian Red Crescent

Domestic

The East Azerbaijan province governor announced two days of public mourning in the province. Mostafa Mohammad Najjar, Minister of Interior and Marzieh Vahid Dastjerdi, Minister of Health, traveled to Tabriz and Ahar. The Iranian Red Crescent did not request any international assistance.[24]

International

In the first two days after the earthquake, the Iranian Red Crescent said they would not accept outside help.[25] Three days after the earthquake, however, the Iranian government announced it would now accept foreign help.[26]

Temporary accommodation tents

Criticism of Iranian government response

The Iranian government was criticised in regarding to its relief efforts. The decision to stop the search for survivors after 24 hours was based on a government assessment that all survivors had been rescued from the rubble; an unnamed local doctor disputed the likelihood of that assessment based on the remoteness of some villages. A lack of tents for the homeless was also cited by members of the Majlis.[44] The IRIB was criticised in an editorial in the Asr-e Iran newspaper for its perceived lack of news coverage of the earthquake. In a Majlis meeting on August 13, 2012, MPs from the affected region questioned President Mahmoud Ahmadinejad for not visiting the area and for not announcing public mourning.[45] That day, Iran then announced two days of public mourning.[46]

References

  1. 1.0 1.1 "Magnitude 6.4 - Northwestern Iran". United States Geological Survey. Retrieved August 11, 2012.
  2. 2.0 2.1 "Two earthquakes in Iran kill 300 and injure 5,000", Ottawa Citizen
  3. 3.0 3.1 3.2 3.3 Zahra Hosseinian (August 12, 2012). "Two quakes in Iran kill 180 and injure 1,500". Reuters. Retrieved August 12, 2012.
  4. 4.0 4.1 "306 killed, 3,037 injured in Iran quakes: Health Mininster", PressTV
  5. "Two deadly earthquakes hit Iran, 250 dead". Deutsche Welle. AP. August 11, 2012. Retrieved August 12, 2012.
  6. 6.0 6.1 Shirzad Bozorgmehr; Michael Martinez (August 11, 2012). "180 killed, 1,300 injured as strong quakes jolt northwestern Iran". CNN. Retrieved August 11, 2012.
  7. RFE/RL (August 11, 2012). "Iranian Official Says 150 Dead In Earthquake". Radio Free Europe/Radio Liberty. Retrieved August 11, 2012.
  8. Talebian, M.; Jackson J. (2004). "A reappraisal of earthquake focal mechanisms and active shortening in the Zagros mountains of Iran" (PDF). Geophysics Journal International (Royal Astronomical Society) 156 (3): 506–526. Bibcode:2004GeoJI.156..506T. doi:10.1111/j.1365-246X.2004.02092.x. Retrieved 12 August 2012.
  9. Allen, M.; Jackson J. & Walker R. (2004). "Late Cenozoic reorganization of the Arabia-Eurasia collision and the comparison of short-term and long-term deformation rates" (PDF). Tectonics (American Geophysical Union) 23. doi:10.1029/2003tc001530. Retrieved 12 August 2012.
  10. Moradi, A.S.; Hatzfeld D. & Tatar M. (2011). "Microseismicity and seismotectonics of the North Tabriz fault (Iran)". Tectonophysics (Elsevier) 506 (1-4): 22–30. Bibcode:2011Tectp.506...22S. doi:10.1016/j.tecto.2011.04.008. Retrieved 12 August 2012.
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  12. USGS (12 August 2012). "M6.4 - 23km SW of Ahar, Iran". Retrieved 12 August 2012.
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  20. UPDATE 2-Two earthquakes in Iran kill 300 and injure 5,000 (Reuters)
  21. 21.0 21.1 Magnitude 5.1 - NORTHWESTERN IRAN
  22. Magnitude 5.0 - NORTHWESTERN IRAN
  23. Magnitude 5.3 - NORTHWESTERN IRAN
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  43. http://www.microsofttranslator.com/BV.aspx?ref=IE8Activity&a=http%3A%2F%2Fpress.catholica.va%2Fnews_services%2Fbulletin%2Fnews%2F29548.php%3Findex%3D29548%26lang%3Den press.catholica.va/news_services/bulletin/news/29548.php?index=29548&lang=en
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  46. Iran announces two days of public mourning
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