1962 Buin Zahra earthquake

The 1962 Buin Zahra earthquake occurred on September 1 in the area of Buin Zahra, Qazvin Province, Iran. The shock had a Richter magnitude of 7.1 and resulted in 12,225 fatalities.[3] Qazvin Province lies in an area of Iran that experiences large earthquakes. The 1962 event originated on one of many faults in the area, called the Ipak Fault. Believed to have been reactivated multiple times, the fault is extensive and could still pose a threat to locals. Iran's building codes, renowned for performing poorly during earthquakes, were recently evaluated by multiple world organizations. Most hope that the Iranian government will implement a better quality of design, highlighting that Iran is among the most seismically active countries in the world.

1962 Buin Zahra earthquake
Tehran
UTC time1962-09-01 19:20:41
ISC event17292570
USGS-ANSSComCat
Local dateSeptember 1, 1962 (1962-09-01)
Local time22:50:41 IRST
Magnitude7.1 ML
Depth10 km (6.2 mi)[1]
Epicenter35.63°N 49.87°E / 35.63; 49.87
FaultIpak Fault
Areas affectedIran
Max. intensityIX (Violent)[2]
Casualtiesat least 12,225 dead, 2,776 injured

Geology

Iran is a seismically active zone, lying between the converging Eurasian and Arabian Plates. Because it has both strike-slip and reverse faults, earthquakes often proceed so that if one fault is overwhelmed by movement, the movement will branch off to another fault, creating a separate earthquake.[4]

Buin Zahra County lies within a zone of active thrust faults, complemented by folds, that extends south from the Alborz mountains.[5] Despite the presence of faults, Qazvin Province does not regularly experience earthquakes. However, the space between earthquakes allows pressure to build up on faults, increasing the power – and magnitude – of the earthquakes.[6]

Specifically, the 1962 event originated on the Ipak Fault of northern Iran, along which it and aftershocks cut roughly 64 miles (103 km) of west-northwest trending surface faulting.[7] A feature that extends for 64 miles (103 km) with its connected, smaller faults, the fault runs from the village of Ipak to Takhrijin. Iranian geologist Manuel Berberian's research indicates that the Ipak Fault is at least as old as the Carboniferous period, and has probably been reactivated several times since its formation. On the fault's south side, Carboniferous material is visible; this debris is not evident on the north side, which suggests that the fault was acting as a "dividing fault" while the area around it underwent sedimentation. Berberian could find no trace of Upper Guadalopian or Julfian sediments north of the fault. Another possible reason for this anomaly could be erosion; uplift could have exposed the northern portion of the fault but not the south.[8]

Damage and casualties
"Actie Herbouw Perzisch Dorp Dousadj"
("action rebuilding of the Persian village Dousadj") organized by the Dutch people

12,225 fatalities resulted from the earthquake. An additional 2,776 people were injured, along with 21,310 houses either destroyed or too damaged to repair. 35 percent of domestic livestock was also killed, and several landslides and rock falls followed the rupture.[7] 21,000 houses were destroyed, mainly because they were made up of mud and brick. Over 7,500 were buried in 31 individual villages, followed by reports from 60 additional villages. In these villages, however, 26,618 survived. One hospital in Tehran was "packed" with over 2,500 victims.[9]

Slight damage was experienced in Tehran, the nation's capital. Cities as far away as Tabriz, Esfahan and Yazd reported the tremor. Sandblows also formed along the rupture zone. The earthquake was also declared the largest rupture in the region since approximately 1630. Multiple reports came from the Rudak area of earthquake lights.[10]

Relief efforts
Gholamreza Takhti and students organized relief efforts.

Rescue operators suggested that an aerial and on-land search should be initiated to help victims. Officials expressed worries that people had gone for over a week with no aid.[11] Iranian wrestling star Gholamreza Takhti gathered blankets, money, and food for victims and transported them by trucks.[12] Because government response was slow, students at the University of Tehran took matters into their own hands. After gathering supplies, the students organized an effort to dispatch medical students and interns to the site of the disaster. Their teams were however blocked by Iranian National Guard members who had been commanded to kill any civilians who tried to help victims; writer Marcello di Cintio cites in Poets and Pahlevans: A Journey into the Heart of Iran that the "Shah was not about to let a crowd of students draw attention to his inept relief efforts".[13]

Future threats

Since roughly 90 percent of Iran lies within seismically active land, the threat from earthquakes is high. In 2002, an earthquake in Buin Zahra killed more than 250 people and left roughly 25,000 without homes.[14]

In addition to its geological threat, Iran has poor earthquake engineering. In a 2004 report by ScienceDaily, it was listed as "the worst offender" globally for poor earthquake engineering.[15] Professor Roger Bilham of the University of Colorado at Boulder, a geophysicist who specializes in earthquake-related deformation and hazards, blames construction practices for the fact that since the start of the 20th century, 1 in 3,000 Iranians has died in an earthquake-related incident. Bilham adds, "Most of Iran needs rebuilding. If the population of Iran had a choice between spending oil revenues on munitions or houses that won't kill them, I suspect they would choose a safe home. It's all a matter of earthquake education."[15] A Common Country Assessment by The United Nations for Iran has similar results, stating that, "While adequate building regulations exist for large cities, it is generally believed that they are not rigorously adhered to... most of those who have suffered in recent major earthquakes have lived in small towns and villages. Earthquake-proof construction is very rare in those areas and adequate building regulations are not yet in place".[16]

gollark: Huh, I skimread that as "at least" and got completely the wrong idea.
gollark: I think this is one of those things where relative ability matters more than absolute ability.
gollark: It seems that some people are consistently more likeable across domains, for whatever reason.
gollark: "Magically be likeable to people who have power in whatever area you're doing stuff" in then.
gollark: Make sure to not leave it too long or it'll disassemble itself into yeast and... bread... components.

See also

Bibliography
  • Ambraseys, N. N. (July 1, 1963). "The Buyin-Zara (Iran) earthquake of September, 1962 a field report". Bulletin of the Seismological Society of America. 53 (4): 705. Archived from the original on July 12, 2011.CS1 maint: ref=harv (link)
  • Berberian, Manuel (1976). "The 1962 Earthquake and Earlier Deformations Abong (sic) the Ipak Earthquake Fault" (PDF). Geological Survey of Iran. 39: 419–427. Retrieved March 21, 2010.CS1 maint: ref=harv (link)
  • Mostafazadeh, Mehrdad; Mokhtari, Mohammad (2003). "Source Time Function of Caspian Basin and Surrounding Area Earthquakes" (PDF). 5 (3). International Institute of Earthquake Engineering and Seismology (IIEES). Archived from the original (PDF) on September 28, 2011. Retrieved June 23, 2011. Cite journal requires |journal= (help)CS1 maint: ref=harv (link)

References
  1. Mostafazadeh & Mokhtari 2003, p. 2.
  2. Berberian, M. (2014), Earthquakes and Coseismic Surface Faulting on the Iranian Plateau, Developments in Earth Surface Processes (1st ed.), Elsevier, p. 603, ISBN 978-0444632920
  3. "Historic Worldwide Earthquakes". United States Geological Survey. January 29, 2009. Archived from the original on February 21, 2009. Retrieved February 21, 2009.
  4. Berberian, Manuel, and Yeats, Robert S, pp. 120–139.
  5. Walker, R. T.; Bergman, E; Jackson, J; Ghorashi, M; Talebain, M. (2005). "The 2002 June 22 Changureh (Avaj) earthquake in Qazvin province, northwest Iran: epicentral relocation, source parameters, surface deformation and geomorphology". Geophysical Journal International. 160 (2): 707–720. Bibcode:2005GeoJI.160..707W. doi:10.1111/j.1365-246X.2005.02516.x.
  6. "Help too late, say quake survivors". CNN. Time Warner. June 24, 2002. Retrieved March 20, 2010.
  7. Ambraseys 1963, pp. 705–740.
  8. Berberian 1976, p. 420.
  9. "Quake Victims Exceed Fears". Ellensburg Daily Record. September 6, 1962. Retrieved February 22, 2009.
  10. "Earthquakes with 1,000 or More Deaths since 1900". United States Geological Survey. January 29, 2009. Archived from the original on June 14, 2009. Retrieved February 22, 2009.
  11. Jay Walz (September 9, 1962). "Wide Search Is Pressed in Iran For Additional Quake Victims; Rescuers Fear Some in Remote Villages Have Suffered a Week With No Aid --Relief Operations Stepped Up U.S. Copters Join Search Families Won't Separate". New York Times. Retrieved February 22, 2009.
  12. "British Museum Opens New Exhibition, Takhti: A Modern Iranian Hero". ArtDaily. 2007. Retrieved February 21, 2009.
  13. di Cintio, Marcello (2007). Poets and Pahlevans: A Journey into the Heart of Iran. Random House Digital, Inc. p. 272.
  14. "Preliminary Earthquake Reconnaissance Report on the June 22, 2002 Changureh (Avaj), Iran Earthquake". International Institute of Earthquake Engineering and Seismology. July 19, 2002. Archived from the original on March 25, 2010. Retrieved February 19, 2010.
  15. "Contractor Ignorance Kills Earthquake Victims In Sesmic Zones, Says U. Of Colorado Professor". ScienceDaily. ScienceDaily LLC. December 28, 2004. Retrieved October 11, 2009.
  16. "United Nations Common Country Assessment for the Islamic Republic of Iran" (PDF). United Nations. Archived from the original (PDF) on July 19, 2011. Retrieved November 23, 2009.
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