506:
University of
Colorado declared that "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." The United Nations developed a Common Country Assessment for Iran, stating, "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".
406:. The results are consistent with a fault that did not reach the surface. A simple fault plane model with a width of 12.8 km dipping to the southeast makes a reasonable match with the observed uplift pattern. However, the best fit to both the results from body wave modelling and SAR interferometry comes from a model with two contiguous fault segments, one to the northeast with a strike of 025Ā°, and the other to the southwest with a strike of 065Ā°, both with an overall southeasterly dip. It has been suggested that this earthquake and the 2005 Qeshm event may have ruptured adjacent parts of the same fault.
415:
29:
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36:
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large, mainly anticlinal folds that show a variety of trends in the central part of the island. The axis of the Laft anticline runs mainly NW–SE, while the Salakh anticline trends roughly W–E and the Suza anticline and Ramkan syncline trend SW–NE. The island shows clear evidence of recent uplift in the form of
261:, killing seven people and injuring up to 45. Causing both catastrophic and minor damage, the earthquake devastated up to 200 villages throughout southern Iran, but left the port city of Bandar Abbas almost unscathed. Citizens reportedly panicked when the earthquake hit, emptying into the parks of the city and other open areas.
497:. All of the seven reported deaths occurred on Qeshm, with the injured being transferred to Bandar Abbas by boat. There were no reports of damage to oil industry facilities in the area. High-rise buildings in Dubai swayed during the earthquake, causing some of them to be evacuated, but there were no reports of damage.
377:
The island of Qeshm is elongated WSW–ENE, parallel to the coastline and the regional trend of the main fold axes. It is formed of
Neogene sediments apart from a diapir of Hormuz salt that pierces through to the surface at the western end of the island. The sediments are affected by a series of
473:
Though major locations held up well against the earthquake, most villages did not. From Qeshm Island came reports of power outage and minor damage; 100 houses in all of Qeshm were damaged between 30 and 50 percent. Two-hundred villages were devastated by the earthquake's velocity. Walls in the
398:
The earthquake had a magnitude of 5.9 on the moment magnitude scale, making it the largest in the region since 2005. The hypocentral depth is estimated as 8 km from body wave modelling. The calculated focal mechanism indicates reverse faulting with a small component of strike-slip, on two
505:
As the world's worst in a 2004 report on countries with poor earthquake engineering, Iran is especially prone to earthquakes. In addition, poor construction practice has exacerbated death tolls; 1 in 3,000 Iranians has died in an earthquake-related incident. Roger Bilham, a professor at the
481:
The earthquake posed a threat to all of Bandar Abbas' oil companies, as well as at least one highly productive and expensive refinery at the time of the earthquake. Because of past earthquakes, including one in 2006, many of the city's homes had been rebuilt and outfitted with
929:
Nissen, E.; Yamini-Fard, F.; Tatar, M.; Gholamzadeh, A.; Bergman, E.; Elliott, J.R. (June 2010). "The
Vertical Separation of Mainshock Rupture and Microseismicity at Qeshm Island in the Zagros Fold-and-Thrust Belt, Iran".
434:
reported 15 injured; its homes were constructed from earthquake-resistant material. The earthquake was felt throughout southern Iran, causing slight to moderate damage.
478:
were leveled; all were reduced by the earthquake to debris. Relief workers were sent to rescue any residents from their homes if they had been caught under debris.
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382:, with the highest terrace identified at 220 meters (720 ft) above sea level. An uplift rate of 0.2 millimeters annually has been estimated from
1229:
674:
358:
at some of the weaker layers, leading to folds at different stratigraphic levels have different locations, orientations or wavelengths. Earthquake
1034:
Sorbi, M. R.; Nilfouroushan, F.; Zamani, A. (2012), "Seismicity patterns associated with the
September 10th, 2008 Qeshm earthquake, South Iran",
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1004:
Lohman, R. B.; Barnhart, W. D. (2010), "Evaluation of earthquake triggering during the 2005-2008 earthquake sequence on Qeshm Island, Iran",
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designs. The major oil refinery did not sustain damage, according to
Hojjatollah Ghanimifard, the vice-president of investment affairs for
28:
281:; near Qeshm the rate of convergence is about 25 millimeters annually. Part of this convergence is accommodated by shortening within the
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884:"The 2005 Qeshm Island Earthquake (Iran)āA Link Between Buried Reverse Faulting And Surface Folding in the Zagros Simply Folded Belt?"
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The effects were concentrated on Qeshm, where several buildings were destroyed, although minor damage was reported around
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598:"UAE's National Seismic Network detects 17 tremors". United Arab Emirates News Agency. 12 September 2008.
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963:"A reappraisal of earthquake focal mechanisms and active shortening in the Zagros mountains of Iran"
825:"Contractor Ignorance Kills Earthquake Victims in Sesmic (sic) Zones, Says U. Of Colorado Professor"
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1589:
620:
475:
882:
Nissen, Edwin; Ghorashi, Manoucher; Jackson, James; Parsons, Barry; Talebian, Morteza (May 2007).
289:. The most active part of the Zagros is the 'Simply Folded Belt', which is characterised by large
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704:"1st killer quake in 2Ā½ years leaves 7 dead". Iran Times International. 19 September 2008.
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The earthquake occurred at 3:00 pm local time and was followed by up to seventeen
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depths show that shortening is accommodated by a mixture of high-angle and low-angle
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431:
430:, fatalities from the tremor were limited to Qeshm Island; 30 people were injured.
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possible fault planes, either dipping 43Ā° to the north or 52Ā° to the southeast.
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847:"United Nations Common Country Assessment for the Islamic Republic of Iran"
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age, known together as the 'Competent Group' due to their relatively high
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two years prior had caused damage. The earthquake measured 5.9 on the
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370:, within either the lowest part of the sedimentary cover or in the
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427:
426:. The main shock lasted at least 30 seconds. According to the
402:
Uplift associated with the earthquake has been measured using
315:. The sedimentary rocks above the salt layer comprise a basal
307:, which locally reaches the surface in the crests of some
339:
and interbedded limestones of latest
Cretaceous to Lower
1077:
241:
of southern Iran, 850 kilometres (528 mi) south of
619:. Xinhua News Agency. 11 September 2009. Archived from
1391:
indicates earthquake resulting in at least 30 deaths
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335:, followed by a sequence of mechanically weaker
1396:indicates the deadliest earthquake of the year
1419:
1107:
49:
8:
1006:Journal of Geophysical Research: Solid Earth
617:"Strong earthquake in southern Iran kills 4"
18:
1426:
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539:
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354:. There is evidence of intermediate level
245:. Its epicenter was near the port city of
17:
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801:"Comments for the Significant Earthquake"
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1036:International Journal of Earth Sciences
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718:. Al Jazeera English. 11 September 2008
669:
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470:in Qatar also reported the earthquake.
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638:
319:conglomerate and a thick sequence of
269:Iran lies within the complex zone of
7:
933:Earth and Planetary Science Letters
892:Earth and Planetary Science Letters
744:. 10 September 2008. Archived from
1078:International Seismological Centre
961:Talebian, M.; Jackson, J. (2004).
772:"Earthquake strikes southern Iran"
646:"Earthquake strikes southern Iran"
14:
967:Geophysical Journal International
675:"Significant Earthquakes of 2008"
988:10.1111/j.1365-246X.2004.02092.x
914:10.1111/j.1365-246X.2007.03514.x
852:. United Nations. Archived from
797:National Geophysical Data Center
716:"Deadly earthquake strikes Iran"
237:occurred on 10 September in the
48:
34:
27:
827:. LiveScience. 28 December 2004
679:United States Geological Survey
203:
1585:1968 Dasht-e Bayaz and Ferdows
681:. 16 July 2008. Archived from
35:
1:
1811:September 2008 events in Iran
1801:History of Hormozgan province
543:Talebian et al., pp. 506ā526.
390:from corals on the terraces.
293:formed above a layer of late
570:Nissen et al. 2007, pp. 2ā3.
488:National Iranian Oil Company
588:Nissen et al. 2010, p. 192.
579:Nissen et al. 2010, p. 190.
561:Nissen et al. 2010, p. 183.
521:List of earthquakes in Iran
516:List of earthquakes in 2008
418:USGS ShakeMap for the event
283:Zagros fold and thrust belt
1832:
954:10.1016/j.epsl.2010.04.049
1760:2022ā2023 West Azerbaijan
1386:
1056:10.1007/s00531-012-0771-6
552:Nissen et al. 2007, pg 2.
374:beneath the Hormuz salt.
23:
652:. BBC. 10 September 2008
1540:1923 Torbat-e Heydarieh
946:2010E&PSL.296..181N
141:8 km (5.0 mi)
1816:2008 disasters in Iran
484:seismically engineered
419:
255:moment magnitude scale
770:(10 September 2008).
450:, and intensity III (
417:
410:Damage and casualties
384:Uranium series dating
235:2008 Qeshm earthquake
19:2008 Qeshm earthquake
1765:2024 Razavi Khorasan
1740:2019 East Azerbaijan
1700:2012 East Azerbaijan
1027:10.1029/2010JB007710
748:on 15 September 2008
623:on 13 September 2008
1796:Earthquakes in Iran
1735:2018 Sarpol-e Zahab
1435:Earthquakes in Iran
1126:Earthquakes in 2008
1048:2012IJEaS.101.2215S
1018:2010JGRB..11512413L
979:2004GeoJI.156..506T
905:2007GeoJI.171..326N
742:National Geographic
442:) were assigned to
163: /
68:2008-09-10 11:00:34
20:
1630:1990 ManjilāRudbar
1086:authoritative data
420:
404:SAR interferometry
265:Geological setting
259:surface wave scale
239:HormozgÄn Province
227:7 dead, 45 injured
1773:
1772:
1650:2002 Bou'in-Zahra
1401:
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231:
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167:26.743Ā°N 55.828Ā°E
102:10 September 2008
1823:
1786:2008 earthquakes
1695:2010 Hosseinabad
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738:"Week in Photos"
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1012:(B12): B12413,
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998:Further reading
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16:
1806:Bandar Abbas
1791:2008 in Iran
1725:2014 Murmuri
1715:2013 Saravan
1710:2013 Bushehr
1690:2010 Damghan
1679:
1660:2004 Baladeh
1640:1997 Ardabil
1635:1997 Bojnurd
1615:1979 Ghaenat
1509:1879 Bozqush
1469:1679 Yerevan
1393:
1388:
1377:SkƄne County
1343:
1330:(6.4, Oct 6)
1322:
1321:(6.6, Oct 5)
1301:
1285:
1284:(~6, Aug 30)
1226:(6.5, Jun 8)
1195:
1158:Market Rasen
1146:
1145:(5.9, Feb 3)
1082:bibliography
1039:
1035:
1009:
1005:
970:
966:
937:
931:
918:. Retrieved
896:
890:
875:Bibliography
874:
873:
861:. Retrieved
854:the original
841:
829:. Retrieved
804:. Retrieved
791:
779:. Retrieved
775:
762:
750:. Retrieved
746:the original
732:
720:. Retrieved
710:
699:
687:. Retrieved
683:the original
654:. Retrieved
649:
625:. Retrieved
621:the original
593:
584:
575:
566:
557:
548:
504:
495:Bandar Abbas
492:
480:
472:
451:
439:
432:Qeshm Island
421:
401:
397:
376:
313:salt diapirs
273:between the
268:
247:Bandar Abbas
234:
232:
213:
187:Oblique-slip
15:
1665:2005 Zarand
1620:1981 Golbaf
1600:1977 Naghan
1595:1977 Khurgu
1570:1957 Alborz
1550:1930 Salmas
1519:1895 Quchan
1514:1893 Quchan
1499:1853 Shiraz
1489:1780 Tabriz
1484:1778 Kashan
1479:1727 Tabriz
1474:1721 Tabriz
1464:1641 Tabriz
1454:893 Ardabil
1449:856 Damghan
1259:Chino Hills
1224:Peloponnese
1201:El Calvario
1042:(8): 2215,
863:23 November
806:30 December
781:30 December
722:10 February
656:10 February
474:village of
424:aftershocks
364:hypocentral
249:, where an
170: /
76: event
1780:Categories
1705:2012 Zohan
1680:2008 Qeshm
1670:2005 Qeshm
1645:1997 Qayen
1625:1981 Sirch
1610:1978 Tabas
1565:1953 Torud
1494:1840 Ahora
1442:Historical
1319:Kyrgyzstan
1247:Dodecanese
831:11 October
527:References
394:Earthquake
356:detachment
348:sandstones
333:competence
325:Palaeozoic
321:limestones
309:anticlines
251:earthquake
224:Casualties
212:MMI VIII (
158:55Ā°49ā²41ā³E
155:26Ā°44ā²35ā³N
106:2008-09-10
65: time
1745:2020 Khoy
1295:September
1282:Panzhihua
1276:Yingjiang
1143:Lake Kivu
1064:128416078
456:Abu Dhabi
388:aragonite
271:collision
206:intensity
146:Epicenter
122:Magnitude
1655:2003 Bam
1590:1972 Qir
1370:December
1360:Sulawesi
1353:November
1340:Pakistan
1334:Chechnya
1175:Illinois
1152:Simeulue
1136:February
776:BBC News
752:26 April
689:26 April
650:BBC News
627:26 April
510:See also
436:Mercalli
372:basement
317:Cambrian
277:and the
80:13393964
1328:Damxung
1312:October
1207:Iceland
1192:Sichuan
1084:and/or
1044:Bibcode
1014:Bibcode
975:Bibcode
942:Bibcode
901:Bibcode
476:Zeynabi
464:Sharjah
345:Neogene
341:Miocene
104: (
1528:Modern
1269:August
1080:has a
1062:
920:2 July
462:, and
302:Hormuz
243:Tehran
214:Severe
93:ComCat
42:Tehran
1302:Qeshm
1253:Iwate
1230:Iwate
1168:April
1060:S2CID
887:(PDF)
857:(PDF)
850:(PDF)
460:Dubai
444:Ajman
440:Light
337:marls
291:folds
138:Depth
117:06:30
86:USGS-
1240:July
1217:June
1076:The
922:2011
865:2009
833:2009
808:2012
783:2012
754:2009
724:2010
691:2009
658:2010
629:2009
468:Doha
452:Weak
446:and
362:and
350:and
305:salt
233:The
204:Max.
197:Iran
183:Type
125:5.9
88:ANSS
1185:May
1052:doi
1040:101
1022:doi
1010:115
983:doi
971:156
950:doi
938:296
909:doi
897:171
768:BBC
428:BBC
386:of
327:to
323:of
311:as
297:to
74:ISC
63:UTC
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1394:ā”
1196:ā ā”
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130:w
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
