248:
violent, it damaged several nearby villages around the three aforementioned cities. These ]s had their own sequences of ]s with the largest measuring 4.7 and the ] on 16 August was preceded by a magnitude 4.5 shock two hours prior. These earthquakes caused panic among the populations and some were damaging. Tourists of ] fled the city following these foreshocks. The last felt foreshock also caused minor damage to villages.<ref name="Ambraseys74">{{cite journal |last1=Ambraseys |first1=N.N. |last2=Moinfar |first2=A.A. |title=The seismicity of Iran. The
Firuzabad (Nehavend) earthquake of 16 August 1958 |journal=Annals of Geophysics |date=1974 |volume=27 |issue=1-2 |pages=1â21 |doi=10.4401/ag-4910}}</ref>{{rp|p=2â6}}
240:
violent, it damaged several nearby villages around the three aforementioned cities. These ]s had their own sequences of ]s with the largest measuring 4.7 and the ] on 16 August was preceded by a magnitude 4.5 shock two hours prior. These earthquakes caused panic among the populations and some were damaging. Tourists of ] fled the city following these foreshocks. The last felt foreshock also caused minor damage to villages.<ref name="Ambraseys74">{{cite journal |last1=Ambraseys |first1=N.N. |last2=Moinfar |first2=A.A. |title=The seismicity of Iran. The
Firuzabad (Nehavend) earthquake of 16 August 1958 |journal=Annals of Geophysics |date=1974 |volume=27 |issue=1-2 |pages=1â21 |doi=10.4401/ag-4910}}</ref>{{rp|p=2â6}}
278:
homes crumbled when an aftershock struck in the early morning of 19 August. The most destructive aftershock occurred in ] on 21 September, devastating a {{cvt|100|km2}} region northwest of the 1957 meizoseismal area. Preceded by a damaging sequence of earthquakes several hours earlier, this magnitude 5.2 shock killed 16 people and devastated ], ], ], Gamshah, and ]. Fifty-seven injuries were reported in the villages of
Karkasar and Karaj. Homes in Karaj sustained damage including fractured walls and one home was destroyed in the prior earthquake sequence.<ref name="Ambraseys74" />{{rp|p=16}}
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homes crumbled when an aftershock struck in the early morning of 19 August. The most destructive aftershock occurred in ] on 21 September, devastating a {{cvt|100|km2}} region northwest of the 1957 meizoseismal area. Preceded by a damaging sequence of earthquakes several hours earlier, this magnitude 5.2 shock killed 16 people and devastated ], ], ], Gamshah, and ]. Fifty-seven injuries were reported in the villages of
Karkasar and Karaj. Homes in Karaj sustained damage including fractured walls and one home was destroyed in the prior earthquake sequence.<ref name="Ambraseys74" />{{rp|p=16}}
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6.7 earthquake occurred at a depth of 15 km (9.3 mi) on 16 August at 22:43 local time. It caused severe damage to over 170 villages in the province. Due to several strong foreshocks, most of the population fled their homes and the death toll only stood at 132 and another 948 were injured. A
247:
Aftershock activity associated with the 13 December 1957 ] continued until mid-February 1958. On 14 August, at 14:00 local time, earthquake activity resumed with a magnitude 5.7 event that was felt strongly in ], ] and ] and scared residents. A magnitude 5.5 earthquake occurred at 19:30; described as
239:
Aftershock activity associated with the 13 December 1957 ] continued until mid-February 1958. On 14 August, at 14:00 local time, earthquake activity resumed with a magnitude 5.7 event that was felt strongly in ], ] and ] and scared residents. A magnitude 5.5 earthquake occurred at 19:30; described as
662:
of Arabia while the rocks to the northeast are of metamorphic and volcanic origin. Its southeastern segments ends in a zone of northânorthwest trending strike-slip faults. The strike-slip component of this oblique convergence is accommodated along the Main Recent Fault. The southeastern segments are
277:
The mainshock was followed by three large aftershocks exceeded magnitude 5.0 while another 30 had magnitudes between 4.0 and 4.9. On 17 August a damaging ] occurred in the
Kangavar area. It left several homes damaged in Kangavar and two more in ]. Several people died in Asadabad and Akbarabad when
269:
The mainshock was followed by three large aftershocks exceeded magnitude 5.0 while another 30 had magnitudes between 4.0 and 4.9. On 17 August a damaging ] occurred in the
Kangavar area. It left several homes damaged in Kangavar and two more in ]. Several people died in Asadabad and Akbarabad when
760:
produced up to 2 m (6 ft 7 in) of vertical offset. The rupture extended across the Garrin segment to the southeast and Sahneh segment to the northwest. The
Nahavand segment was associated with another 20 km (12 mi) surface rupture that extended form
166:
801:
The mainshock killed at least 132 people, injured hundreds and killed 3,000 livestock. Approximately 2,500 homes across 170 villages were levelled, rendering 10,000 homeless. The low death toll was partly the result of a foreshock that kept residents alert and the
837:, these villages were also affected by the 1957 earthquake and its aftershocks. There, all homes were razed, and in Leylas, cows were knocked off their feet and residents had difficulty maintaining their balance. About 200 died or were injured in these villages.
856:, two people died from toppled adobe walls; several damaged homes were restored after the 1957 shock. The village of Dehkuhneh was in the process of reuilding after the 1957 shock when it was completely devastated again; there were two deaths and 23 injuries.
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buildings as these structures do not remain intact beyond intensity VII. Some infrastructure in the meizoseismal zone had been damaged by the 1957 shock and its aftershock which could not be distinguished from actual damage caused by the 1958 earthquake.
1079:
Rahimzadeh, Bahman; Bahrami, Shahram; Mohajjel, Mohammad; Mahmoudi, Hossein; Haj-Azizi, Farzad (2019). "Active strike-slip faulting in the Zagros
Mountains: Geological and geomorphological evidence of the pull-apart Zaribar Lake basin, Zagros, NW Iran".
60:
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on 21 September, devastating a 100 km (39 sq mi) region northwest of the 1957 meizoseismal area. Preceded by a damaging sequence of earthquakes several hours earlier, this magnitude 5.2 shock killed 16 people and devastated
650:, to the northeast, seismicity is nearly absent. The Main Recent Fault delineates the northeastern boundary of the Zagros Mountains, forming between 3 and 5 million years ago. It runs parallel to the Main Zagros Reverse Fault, a
642:
between the
Arabian Plate and Iran occurs obliquely along the Zagros Mountains, and approximately 30â50 percent of the ~25 cm (9.8 in) per year convergence between the two plates is accommodated along the range.
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may have occurred. The mountain range is still accommodating deformation, evident from present-day seismicity. Deformation is accommodated by thrust and strike-slip faulting within the range. Parallel to major
872:, persisted for a while and many people could not walk properly. One home also collapsed in the city and buried a person. Three people died and nine were injured in the flattened town of Barfaragh.
740:. Fifty-seven injuries were reported in the villages of Karkasar and Karaj. Homes in Karaj sustained damage including fractured walls and one home was destroyed in the prior earthquake sequence.
15:
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The mainshock and its aftershocks occurred southeast of the 1957 earthquake epicenter. Both earthquakes occurred along different segments of the Main Recent Fault. Three sets of
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719:. Several people died in Asadabad and Akbarabad when homes crumbled when an aftershock struck in the early morning of 19 August. The most destructive aftershock occurred in
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and scared residents. A magnitude 5.5 earthquake occurred at 19:30; described as violent, it damaged several nearby villages around the three aforementioned cities. These
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occurred; all trending northwestâsoutheast on segments of the Main Recent Fault exhibited vertical offsets. One of these ran 15 km (9.3 mi) between
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on 16 August was preceded by a magnitude 4.5 shock two hours prior. These earthquakes caused panic among the populations and some were damaging. Tourists of
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The mainshock was followed by three large aftershocks exceeded magnitude 5.0 while another 30 had magnitudes between 4.0 and 4.9. On 17 August a damaging
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1159:
Developments in Earth
Surface Processes] Earthquakes and Coseismic Surface Faulting on the Iranian Plateau - A Historical, Social and Physical Approach
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continued until mid-February 1958. On 14 August, at 14:00 local time, earthquake activity resumed with a magnitude 5.7 event that was felt strongly in
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and Litagar, situated in the northwest meizoseismal zone, experienced the greatest devastation. Located some 10 km (6.2 mi) from
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The earthquake was felt for 180,000 km (69,000 sq mi); a significantly larger extent in comparison with the 1957 shock.
658:. The fault comprises several segments with lengths of more than 100 km (62 mi). Southwest of the Main Recent Fault lies the
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995:
Tchalenko, J. S.; Braud, J. (1974). "Seismicity and structure of the Zagros (Iran): the Main Recent Fault between 33 and 35° N".
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Ambraseys, N.N.; Moinfar, A.A. (1974). "The seismicity of Iran. The Firuzabad (Nehavend) earthquake of 16 August 1958".
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1032:"Microearthquake seismicity at the intersection between the Kazerun fault and the Main Recent Fault (Zagros, Iran)"
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fled the city following these foreshocks. The last felt foreshock also caused minor damage to villages.
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Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences
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districts. The meizoseismal area encompassed a 1,100 km (420 sq mi) area along the
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occurred in the Kangavar area. It left several homes damaged in Kangavar and two more in
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of the mountains is the Main Recent Fault, an active right-lateral
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was damaged by landslides and slumps. All homes were flattened in
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more seismically active in contrast to the northwestern segments.
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destructive aftershock on 21 September killed another 16 people.
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The northeast-trending Main Recent Fault in the Zagros Mountains
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Yamini-Fard, F.; Hatzfeld, D.; Tatar, M.; Mokhtari, M. (2006).
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ISC-GEM Global Instrumental Earthquake Catalogue (1900â2009)
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788:) effects. It was impossible to further assess the damaged
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Aftershock activity associated with the 13 December 1957
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although there were plausibly isolated instances of IX (
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The Zagros Mountains is seismically active while in the
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indicates earthquake resulting in at least 30 deaths
1157:(2014). "12: 1900â1963 Coseismic Surface Faulting".
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1638:indicates the deadliest earthquake of the year
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313:Latest revision as of 00:30, 23 September 2024
158:Latest revision as of 00:30, 23 September 2024
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2053:History of Kermanshah province
1822:1968 Dasht-e Bayaz and Ferdows
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18:Browse history interactively
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2043:History of Hamadan province
887:List of earthquakes in Iran
882:List of earthquakes in 1958
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1977:2019 East Azerbaijan
1937:2012 East Azerbaijan
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1128:Annals of Geophysics
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877:
874:
823:Gamasiab River
798:
795:
745:
742:
673:
670:
668:
665:
597:involving the
571:Main article:
568:
565:
557:
537:
536:
533:
529:
528:
525:
521:
520:
517:
513:
512:
499:
492:
491:
486:
485:Areas affected
482:
481:
474:34.290; 47.867
449:
445:
444:
441:
437:
436:
431:
425:
421:
420:
417:
413:
412:
408:16 August 1958
404:16 August 1958
402:
398:
397:
392:
385:
384:
379:
372:
371:
368:
361:
360:
352:
351:
344:
343:
335:
334:
328:
327:
326:
316:
314:
309:
308:
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296:
293:
292:
289:
287:
284:
281:
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268:
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259:
257:
254:
251:
250:
246:
244:
242:
238:
236:
233:
232:
229:
225:
224:
203:
190:
189:
174:
153:
127:
114:
113:
98:
67:
61:
59:
41:
33:
27:
23:
22:
14:
9:
6:
4:
3:
2:
2065:
2054:
2051:
2049:
2046:
2044:
2041:
2039:
2036:
2034:
2031:
2029:
2026:
2024:
2021:
2020:
2018:
2003:
2000:
1998:
1995:
1993:
1990:
1988:
1985:
1983:
1980:
1978:
1975:
1973:
1970:
1968:
1965:
1963:
1960:
1958:
1957:2013 Borazjan
1955:
1953:
1950:
1948:
1945:
1943:
1940:
1938:
1935:
1933:
1930:
1928:
1925:
1923:
1920:
1918:
1915:
1913:
1912:2006 Borujerd
1910:
1908:
1905:
1903:
1900:
1898:
1895:
1893:
1890:
1888:
1885:
1883:
1880:
1878:
1875:
1873:
1870:
1868:
1865:
1863:
1860:
1858:
1855:
1853:
1850:
1848:
1845:
1843:
1840:
1838:
1835:
1833:
1830:
1828:
1825:
1823:
1820:
1818:
1815:
1813:
1812:1957 Farsinaj
1810:
1808:
1805:
1803:
1800:
1798:
1797:1948 Ashgabat
1795:
1793:
1792:1947 Dustabad
1790:
1788:
1785:
1783:
1780:
1778:
1775:
1773:
1772:1909 Borujerd
1770:
1769:
1767:
1763:
1757:
1754:
1752:
1749:
1747:
1744:
1742:
1739:
1737:
1734:
1732:
1729:
1727:
1724:
1722:
1719:
1717:
1714:
1712:
1709:
1707:
1704:
1702:
1701:1667 Shamakhi
1699:
1697:
1694:
1692:
1689:
1688:
1686:
1682:
1678:
1671:
1666:
1664:
1659:
1657:
1652:
1651:
1648:
1637:
1632:
1627:
1621:
1617:
1614:
1612:(6.4, Aug 26)
1611:
1610:Coatzacoalcos
1608:
1606:(7.1, Aug 15)
1605:
1602:
1599:
1596:
1595:
1593:
1591:
1587:
1581:
1578:(6.7, Aug 16)
1577:
1574:
1571:
1568:
1565:
1562:
1560:
1556:
1553:
1552:
1550:
1548:
1544:
1538:
1534:
1531:
1528:
1525:
1523:
1519:
1516:
1514:
1510:
1507:
1505:
1501:
1498:
1495:
1492:
1489:
1488:San Francisco
1486:
1483:
1480:
1479:
1477:
1475:
1471:
1465:
1461:
1458:
1456:
1452:
1449:
1447:
1443:
1440:
1438:
1434:
1431:
1429:
1425:
1422:
1420:(5.0, Apr 19)
1419:
1416:
1414:
1410:
1407:
1405:(5.8, Jan 12)
1404:
1401:
1400:
1398:
1396:
1392:
1386:
1383:(6.7, Sep 9)
1382:
1379:
1377:(7.1, Dec 16)
1376:
1375:Fairview Peak
1373:
1371:
1367:
1364:
1361:
1358:
1357:
1355:
1353:
1349:
1343:(7.5, Dec 12)
1342:
1339:
1336:
1333:
1331:
1327:
1324:
1322:
1318:
1315:
1312:
1309:
1307:
1303:
1300:
1298:
1294:
1291:
1290:
1288:
1286:
1282:
1276:
1273:(9.0, Nov 5)
1272:
1269:
1267:
1263:
1260:
1257:
1254:
1251:
1248:
1246:
1242:
1239:
1237:
1234:(5.8, Jan 3)
1233:
1230:
1229:
1227:
1225:
1221:
1212:
1207:
1205:
1200:
1198:
1193:
1192:
1189:
1178:
1172:
1168:
1164:
1160:
1156:
1149:
1141:
1137:
1134:(1â2): 1â21.
1133:
1129:
1122:
1120:
1118:
1116:
1114:
1112:
1103:
1099:
1095:
1091:
1087:
1083:
1075:
1067:
1063:
1058:
1053:
1049:
1045:
1041:
1037:
1033:
1026:
1018:
1014:
1010:
1006:
1002:
998:
991:
983:
977:
964:
960:
956:
952:
948:
947:
939:
924:
920:
916:
915:
907:
905:
903:
898:
888:
885:
883:
880:
879:
873:
871:
867:
863:
859:
855:
851:
847:
843:
838:
836:
832:
828:
824:
820:
816:
812:
807:
805:
794:
791:
787:
783:
779:
775:
770:
768:
764:
763:Barreh Farakh
759:
758:Cheshmeh Mahi
755:
751:
741:
739:
735:
731:
727:
722:
718:
714:
709:
707:
703:
699:
695:
691:
687:
683:
679:
664:
661:
657:
653:
649:
644:
641:
637:
633:
632:thrust faults
628:
624:
620:
616:
612:
608:
604:
600:
599:Arabian Plate
596:
592:
588:
579:
574:
564:
561:
552:
548:
544:
534:
530:
526:
522:
518:
514:
510:
507:
500:
493:
490:
487:
483:
478:
450:
446:
442:
438:
435:
426:
422:
418:
414:
403:
399:
396:
393:
391:
386:
383:
380:
377:
373:
369:
366:
362:
332:
324:
312:
304:
302:
297:
295:
294:
290:
288:
285:
283:
282:
275:
267:
264:
260:
258:
255:
253:
252:
245:
243:
237:
235:
234:
226:
217:
201:
197:
193:
192:Autopatrolled
186:
182:
177:
168:
163:
159:
151:
141:
125:
121:
117:
116:Autopatrolled
110:
106:
101:
92:
88:
70:
55:
48:
38:Content added
30:
20:
2033:1958 in Iran
1962:2014 Murmuri
1952:2013 Saravan
1947:2013 Bushehr
1927:2010 Damghan
1897:2004 Baladeh
1877:1997 Ardabil
1872:1997 Bojnurd
1852:1979 Ghaenat
1816:
1711:1679 Yerevan
1635:
1630:
1619:
1600:(8.0, May 4)
1579:
1575:
1572:(7.8, Jul 9)
1566:(7.1, Apr 7)
1558:
1536:
1521:
1512:
1503:
1463:
1454:
1445:
1436:
1427:
1412:
1384:
1369:
1362:(5.6, Mar 1)
1329:
1320:
1313:(7.6, May 6)
1305:
1302:YeniceâGĂśnen
1296:
1274:
1265:
1244:
1235:
1158:
1148:
1131:
1127:
1085:
1081:
1074:
1039:
1035:
1025:
1000:
996:
990:
966:, retrieved
949:(Data Set),
945:
938:
927:, retrieved
913:
839:
808:
800:
785:
777:
771:
747:
710:
675:
645:
603:Central Iran
591:Gulf of Oman
584:
542:
540:
505:
1902:2005 Zarand
1857:1981 Golbaf
1837:1977 Naghan
1832:1977 Khurgu
1807:1957 Alborz
1787:1930 Salmas
1756:1895 Quchan
1751:1893 Quchan
1741:1853 Shiraz
1731:1780 Tabriz
1726:1778 Kashan
1721:1727 Tabriz
1716:1721 Tabriz
1706:1641 Tabriz
1696:893 Ardabil
1691:856 Damghan
1616:Hebgen Lake
1424:Afghanistan
1256:Kern County
1088:: 332â345.
804:hot weather
778:Very strong
698:aftershocks
652:suture zone
640:Convergence
636:strike-slip
524:Aftershocks
472: /
378: event
140:ââMainshock
2017:Categories
1942:2012 Zohan
1917:2008 Qeshm
1907:2005 Qeshm
1882:1997 Qayen
1862:1981 Sirch
1847:1978 Tabas
1802:1953 Torud
1736:1840 Ahora
1684:Historical
1570:Lituya Bay
1311:ConcepciĂłn
968:2022-12-05
929:5 December
893:References
850:Sharifabad
846:Hoseynabad
713:aftershock
694:foreshocks
667:Earthquake
615:Cretaceous
549:to strike
547:earthquake
532:Casualties
516:Foreshocks
460:47°52â˛01âłE
457:34°17â˛24âłN
367: time
1982:2020 Khoy
1598:Kamchatka
1576:Firuzabad
1460:Nicaragua
1232:Hasankale
1066:130787307
1017:122302270
862:riverbank
854:Firuzabad
831:Jafarabad
744:Mainshock
717:Karkhaneh
702:mainshock
690:Tuyserkan
619:Oligocene
498:intensity
448:Epicenter
424:Magnitude
1892:2003 Bam
1827:1972 Qir
1604:Hengchun
1533:Farsinaj
1527:Mongolia
1518:Guerrero
1403:Budapest
1360:Adelaide
1250:San Juan
1241:Hokkaido
976:citation
923:archived
876:See also
870:Asadabad
858:Slumping
738:Kolehjub
726:Karkasar
686:Nahavand
682:Asadabad
623:Pliocene
611:Jurassic
607:Triassic
504:MMI IX (
419:22:43:48
231:Line 50:
228:Line 50:
185:contribs
109:contribs
53:Wikitext
1494:Fethiye
1442:Sagaing
1433:Amorgos
1366:Sofades
1262:Damxung
1090:Bibcode
1044:Bibcode
860:of the
842:Rudbari
786:Violent
734:Balajub
706:Hamadan
638:fault.
613:, late-
609:, late-
506:Violent
406: (
1765:Modern
1564:Huslia
1509:Alborz
1341:Tumbes
1326:Cyprus
1317:Ionian
1173:
1064:
1015:
827:Leylan
811:Khezel
767:Laylan
754:Givaki
395:ComCat
382:884953
353:Tehran
205:24,736
129:24,736
64:Inline
46:Visual
1500:Abant
1451:Anjar
1381:Chlef
1293:Torud
1062:S2CID
1013:S2CID
864:near
815:Solgi
790:adobe
776:VII (
730:Karaj
440:Depth
388:USGS-
207:edits
131:edits
1590:1959
1547:1958
1474:1957
1409:Chim
1395:1956
1352:1954
1335:Suva
1285:1953
1224:1952
1171:ISBN
982:link
955:NOAA
931:2022
848:and
817:and
756:and
688:and
621:and
601:and
585:The
541:The
527:Yes
519:Yes
496:Max.
489:Iran
427:6.7
390:ANSS
181:talk
167:undo
162:edit
105:talk
91:edit
1163:doi
1136:doi
1098:doi
1086:174
1052:doi
1040:166
1005:doi
1001:277
959:doi
765:to
376:ISC
365:UTC
2019::
1580:â âĄ
1537:â âĄ
1513:â âĄ
1428:âĄâ
1385:âĄâ
1306:âĄâ
1275:â âĄ
1169:.
1132:27
1130:.
1110:^
1096:.
1084:.
1060:.
1050:.
1038:.
1034:.
1011:.
999:.
978:}}
974:{{
957:,
953:,
921:,
901:^
829:,
813:,
732:,
728:,
684:,
617:,
220:wl
218::
198:,
194:,
183:|
144:ce
142::
122:,
118:,
107:|
1669:e
1662:t
1655:v
1636:âĄ
1631:â
1620:âĄ
1559:â
1522:â
1504:â
1464:â
1455:â
1446:â
1437:â
1413:â
1370:â
1330:â
1321:â
1297:â
1266:â
1245:â
1236:â
1210:e
1203:t
1196:v
1179:.
1165::
1152:{
1142:.
1138::
1104:.
1100::
1092::
1068:.
1054::
1046::
1019:.
1007::
984:)
961::
558:w
556:M
508:)
432:w
430:M
410:)
187:)
179:(
111:)
103:(
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
