1930 Salmas earthquake

The 1930 Salmas earthquake occurred on May 7 at 01:34:26 IRST in West Azerbaijan Province, Iran. The earthquake, which was among Iran's largest, measured 7.1 on the moment magnitude scale and had a maximum Mercalli intensity of IX (Violent). A damaging foreshock occurred fifteen hours prior to the main event and served as a warning to the people that felt it strongly. Reports from seismologists and seismological organizations indicate that up to 3,000 fatalities may have occurred in northwest Iran and southeast Turkey.

1930 Salmas earthquake
Tabriz
Kirkuk
Baghdad
UTC time1930-05-06 22:34:26
ISC event907354
USGS-ANSSComCat
Local dateMay 7, 1930 (1930-05-07)
Local time01:34:26 IRST
Magnitude7.1 Mw [1]
Depth15 km (9.3 mi) [1]
Epicenter38.09°N 44.78°E / 38.09; 44.78 [1]
FaultSalmas Fault [2]
TypeOblique-slip
Areas affectedIran, Turkey
Max. intensityIX (Violent) [3]
LandslidesYes
Foreshocks5.4 mb May 6 at 07:03:26 [4]
Casualties1,360–3,000 killed [5]

Sixty villages (including the large settlement of Dilman, which was relocated and rebuilt as Salmas) were destroyed in the Salmas Plain and in the surrounding mountainous regions. A destructive aftershock sequence affected many villages, and in some cases, damage was inflicted on some that had escaped devastation during the mainshock. An inspection of the region was undertaken, but not until decades later, at which time substantial surface faulting and other ground effects were documented.

Preface

The epicentral area in the Salmas Plain covers 300 square kilometres (120 sq mi) and is positioned northwest of Lake Urmia. This area had been inhabited primarily by Christians for about a thousand years prior to the event (which was one of the largest earthquakes to occur in Iran since 1900). The mountainous areas surrounding the plain are extremely isolated with villages (comprising mainly Kurdish people) that are spread far apart. Montane villagers sustained themselves primarily on wheat and cattle farming. To the west, near the Turkish border, lies Aravil Dagi, a volcano that is the highest peak in the region.[4]

Foreshock

A relatively strong foreshock occurred at about 10:03:26 IRST on May 6 in the same area as the mainshock. This destructive event caused 25 fatalities and was felt as far as northwestern Azerbaijan and southeastern Turkey. Damage to adobe homes was substantial. Roofs and walls collapsed and in some instances whole homes were demolished. Many of the villagers in the valley spent the following night outdoors and were spared during the main event, but in the mountainous villages where the shock was not felt as strongly (Shekar Yazi, Sheydan, Ashnak, Aslanik, and others) the population was not as concerned. Many slept indoors and this led to high casualties in those areas during the mainshock a little more than 15 hours later.[4]

Earthquake
Aftershocks ≥ M5
MDateTime (UTC)
5
May 8
05:29:32
5
May 8
15:05:28
6.25
May 8
15:35:28
5
May 8
23:38:22
5
May 10
21:43:33
5.25
May 23
09:48:23
5.5
May 29
17:14:59
5.25
June 4
07:28:08
5.25
Aug 3
22:05:59
Tchalenko & Berberian 1974, pp. 204, 206

The earthquake was a result of oblique-slip faulting, and was felt over a very wide area, from Leninakan in Armenia and Tbilisi in Georgia in the north, and Baghdad and Kirkuk in Iraq to the south. Dextral strike-slip motion, along with dip-slip motion (normal faulting, northeast side down) occurred on a fault trending west-northwest. The United States' National Geophysical Data Center lists 1,360 fatalities for the event, while the Belgian Centre for Research on the Epidemiology of Disasters' EM-DAT database and Ambraseys & Melville 2005 both list 2,500. Tchalenko & Berberian 1974, the USGS' PAGER loss estimate database, and Utsu 2002 all state 2,514. The Utsu list also acknowledges other estimates of 1,360 and 3,000.[4][5][6]

Damage

Sixty villages and about 40 churches were destroyed in the southwest Salmas Plain and the surrounding mountainous regions. In the zone of heaviest damage (bounded by the villages of Kohneh Shahr, Payajuk and Zaviehjuk) all the homes and all but one of the churches were destroyed. To the east of this area, the large village of Dilman reportedly had 1,100 casualties, but seismologists J. S. Tchalenko and M. Berberian questioned the reliability of this figure. In smaller villages, survivors provided an accurate count of those lost because they remembered the victims by name, but in a village of 18,000, survivors were unable to grasp the extent of the losses. Only two homes remained standing there, and the village was renamed Salmas and moved to a new location to the west.[7]

The villages in the mountains to the south, west, and north of the Salmas Plain were generally smaller, and accounted for about half of the total number of villages that were lost. The foreshock was not felt at Borusliqalan (the westernmost village that was destroyed) and the losses were high. The foreshock was also not strongly felt to the east of Lake Urmia (and to the southwest of Tabriz) where the village of Mamaqan was completely destroyed and 85 people were killed. Other nearby villages went almost unscathed, with the differing amounts of damage being attributed to soil type.[7]

Ground effects

A post-earthquake survey of the land was undertaken by seismologists N. N. Ambraseys and C. P. Melville, but it was not completed until the mid 1970s. At that time, 16 kilometres (9.9 mi) of surface breaks with right-lateral offsets between 1–4 metres (3 ft 3 in–13 ft 1 in) were located between the villages of Shurgil and Kuhneh Shahr. Substantial vertical movement of the west-northwest trending fault was also seen, with even greater maximum displacements of 4–6 metres (13–20 ft), but the average vertical slip was about 1.2 metres (3 ft 11 in) throughout the extent of the observed surface faulting. They estimated that about 30 kilometres (19 mi) of visible fault breaks were present immediately following the shocks, but by the time they had completed their survey 45 years later about half of the surface features had succumbed to erosion. Other effects included disturbed stream and spring flow, water table fluctuations, and landslides.[6]

Aftershocks

A series of strong and damaging aftershocks persisted for about three-and-a-half months. The largest in the sequence came on May 8. The event caused additional destruction to the northeast of the initial meizoseismal area. Qatur, which had been nearly destroyed by the mainshock, took another serious hit. Other villages (Chaliyan, Givaran, Mir 'Umar, and Ravyan) also experienced major destruction. Shekar Yazi was a village in the southeast region that had not been seriously affected by the mainshock, but experienced heavy damage during the May 8 event. This shock resulted in four additional deaths.[6][8]

See also

References
  1. ISC (2015), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009), Version 2.0, International Seismological Centre
  2. Yeats, R. S.; Sieh, K. E.; Allen, C. R. (1997). The Geology of Earthquakes. Oxford University Press. p. 479. ISBN 978-0-19-507827-5.
  3. Berberian, M. (2014), Earthquakes and Coseismic Surface Faulting on the Iranian Plateau, Developments in Earth Surface Processes (1st ed.), Elsevier, p. 595, ISBN 978-0-444-63292-0
  4. Tchalenko & Berberian 1974, pp. 151–155, 159
  5. USGS (September 4, 2009), PAGER-CAT Earthquake Catalog, Version 2008_06.1, United States Geological Survey
  6. Ambraseys, N.N.; Melville, C.P. (2005). A History of Persian Earthquakes. Cambridge University Press. pp. 80, 81. ISBN 978-0-521-02187-6.CS1 maint: ref=harv (link)
  7. Tchalenko & Berberian 1974, pp. 161, 172–186, 209, 210
  8. Berberian, M. (1979), "Tabas-e-Golshan (Iran) catastrohic earthquake of 16 September 1978; A preliminary report" (PDF), Disasters, 2 (4): 212, archived from the original (PDF) on 2017-08-09

Sources

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