1957 Farsinaj earthquake

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1957 Farsinaj earthquake
Iran relief location map.jpg
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Tehran
UTC  time1957-12-13 01:45:04
ISC  event 887684
USGS-ANSS ComCat
Local dateDecember 13, 1957 (1957-12-13)
Magnitude6.5 Mw [1]
Depth15 km (9 mi) [1]
Epicenter 34°23′17″N47°44′53″E / 34.388°N 47.748°E / 34.388; 47.748 [1]
Type Strike-slip
Areas affected Iran
Max. intensity VII (Very strong) +
Casualties1,130 killed

The 1957 Farsinaj earthquake struck Hamadan, Iran on 13 December at 05:15 local time. The moment magnitude 6.5 earthquake destroyed 211 villages, killed approximately 1,130 people, and left another 900 injured. [2]

Contents

Tectonic setting

Geology of the Zagros Mountains ZagrosFTB.png
Geology of the Zagros Mountains

The Zagros Mountains stretching from Turkey to the Gulf of Oman, through Iran and Iraq for 1,500 km (930 mi) formed from continental collision involving the Arabian Plate and Central Iran. Its formation occurred during the late-Triassic, late-Jurassic, late-Cretaceous, Oligocene and Pliocene. During its early formation, some extensional tectonics is believed to have occurred. The mountain range is still accommodating deformation, evident in the present-day seismicity. Deformation is accommodated by thrust and strike-slip faulting within the range. Parallel to major thrust faults of the mountains is the Main Recent Fault, an active right-lateral strike-slip fault. [3] Convergence between the Arabian Plate and Iran occurs obliquely along the Zagros Mountains—approximately 30–50 percent of the ~25 cm (9.8 in)/yr convergence between the two plates is accommodated here. [4]

Earthquake

Three historical earthquakes were documented near the Main Recent Fault. Two earthquakes in May 912 and April 1008 occurred near the former settlement of Dinavar while a third occurred to the southeast of Dorud before 1889. The first two earthquakes brought heavy damage and casualties in Dinawar. Historic records of the 912 earthquake says a "mountain split open" and water gushed out, sinking many settlements. Ground cracks, possibly associated with tectonic origins was documented during the 1008 event. The Main Recent Fault was also associated with the Ms  7.4 earthquake in 1909 which produced more than 40 km (25 mi) of surface rupture. [3]

Seismicity along the Main Recent Fault was nearly absent since 1909. In December 1955, an earthquake near Razan caused rockfalls and three deaths. A single foreshock was felt 26 hours before the mainshock. The mainshock was followed by 32 aftershocks within a month of its occurrence. Its epicenters were instrumentally recorded and located, revealing a northeast—southwest trend intersecting the Main Recent Fault (also perpenticular to the axis of meizoseismal area). [3] Ground deformations including rockfalls and fractures occurred, associated with the mainshock and aftershocks, but there was inconclusive evidence to show that these were of tectonic origin. [5]

Damage and casualties

A site investigation by Nicholas Ambraseys and other researchers revealed serious damage over a 2,800 km2 (1,100 sq mi) area. The earthquake lasted 10 seconds and was felt for 180,000 km2 (69,000 sq mi). Damage was greatest in the northeast than southwest due to the direction that seismic energy radiated. At least 1,130 people died, 900 were injured, and 15,000 became homeless—at least 20,000 animals also died. [5]

The mainshock and its aftershocks heavily damaged or destroyed 5,000 of the 9,000 homes in the area. Most homes were constructed of single-storey adobe or rubble masonry materials held together by mud, and heavy roofs from tampered earth. Some villages had double-storey adobe and single-storey brick homes with jack arches or iron sheets. [6]

In the epicenter area, the seismic intensity was considered modest, assigned VII+ on the Modified Mercalli intensity scale. The area of maximum damage was between Kangavar and Farsinaj, and the most affected areas were north of Sahneh. The severity of damage became inconsistent and repidly fell to the south. No serious damage occurred outside the 15 km (9.3 mi) radius around Farsinaj, and at Sonqor, only cracks appeared in buildings. At Sarab, the village was heavily damaged and 53 residents died, whereas at Sahneh, Gakul and Bisitun, damage was moderate. Northwest of Sahneh the mainshock produced cracks in the ground. Rockfalls and disruption of a natural spring was also recorded. [5]

At Farsinaj, 703 people, or about half the population, perished, and only 30 homes were left intact. The village was reconstructed 1 km (0.62 mi) away from the ruins. At Dehasiyab, 34 people died and 23 were injured—the village was razed and reconstructed several hundred meters away. Six people died, 20 were injured and two-thirds of homes in Sollantaher were destroyed. In two villages north of Farsinaj, the death toll totaled 63. [5]

Aftershocks on 13 and 18 December near Kangavar and Firuzabad on 28 December caused further damage. [3] The aftershock on 14 December caused more than 20 deaths and left 50 injured. Another aftershock on the same day at Najafabad killed one and injured four, and destroyed more buildings. Fourteen people died in an aftershock on 18 December at Fash. An additional 20 people and more animals died from a snow storm on 21 December. On 31 December, another aftershock killed three at Kangavar. [5]

See also

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References

  1. 1 2 3 ISC (27 June 2022), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009), Version 9.1, International Seismological Centre
  2. ↑ National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Database (Data Set), National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K
  3. 1 2 3 4 Tchalenko, J. S.; Braud, J. (1974). "Seismicity and structure of the Zagros (Iran): the Main Recent Fault between 33 and 35° N". Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. 277 (1262): 1–25. doi:10.1098/rsta.1974.0044. S2CID   122302270.
  4. ↑ Yamini-Fard, F.; Hatzfeld, D.; Tatar, M.; Mokhtari, M. (2006). "Microearthquake seismicity at the intersection between the Kazerun fault and the Main Recent Fault (Zagros, Iran)". Geophysical Journal International. 166 (1): 186–196. Bibcode:2006GeoJI.166..186Y. doi: 10.1111/j.1365-246X.2006.02891.x . S2CID   130787307.
  5. 1 2 3 4 5 Ambraseys, N. N.; Moinfar, A. A.; Peronaci, P. (1973). "The Seismieity of Iran the Farsinaj (Kermanshah) earthquake of 13 December 1957". Annals of Geophysics. 26 (4). doi: 10.4401/ag-5030 .
  6. ↑ "Farsinaj Earthquake of 13 December 1957, Ms7.1". International Institute of Earthquake Engineering and Seismology . Retrieved 5 December 2022.
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