1930 Salmas earthquake

From Wikipedia, the free encyclopedia
Jump to: navigation, search
1930 Salmas earthquake
1930 Salmas earthquake is located in Iran
1930 Salmas earthquake
Date May 6 at 22:34:26 UTC [1]
Magnitude 7.1 Mw [1]
Depth 15 km (9.3 mi) [1]
Epicenter 38°05′N 44°47′E / 38.09°N 44.78°E / 38.09; 44.78Coordinates: 38°05′N 44°47′E / 38.09°N 44.78°E / 38.09; 44.78 [1]
Type Oblique-slip
Areas affected Iran, Turkey
Max. intensity X (Extreme) [2]
Landslides Yes
Foreshocks 5.4 Mb May 6 at 07:03:26 [3]
Casualties 1,360–3,000 killed [2]

The 1930 Salmas earthquake occurred on May 7 at 01:34 IRST in West Azerbaijan Province, Iran. The earthquake measured 7.1 on the moment magnitude scale and had a maximum Mercalli intensity of X (Extreme). A damaging foreshock occurred fifteen hours prior to the main event and served as a warning to the villages that felt it strongly. Up to 3,000 fatalities may have occurred in western Iran and eastern Turkey. 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.


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 strongest 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. Mountain 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.[3]


A relatively strong foreshock occurred at about 10 a.m. local time 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 the 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.[3]


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. Right-lateral strike-slip motion, along with dip-slip motion (normal faulting, northeast side down) occurred on a fault trending WNW–ESE. 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's catalog of Persian events both list 2,500. Tchalenko & Berberian's 1974 report, the USGS' PAGER loss estimate database, and Tokuji Utsu's 2002 catalog all state 2,514. The Utsu list also acknowledges other estimates of 1,360 and 3,000.[2][3][4]

Aftershocks ≥ M5
M Date Time (UTC)
May 8
May 8
May 8
May 8
May 10
May 23
May 29
June 4
Aug 3
Tchalenko & Berberian 1974, pp. 204, 206


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 researchers 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.[5]

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 felt strongly 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.[5]

Ground effects[edit]

A post-earthquake survey of the land was not completed until the mid 1970s. At that time, 16 kilometers (9.9 mi)) of surface breaks with right-lateral offsets between 1–4 meters (3 ft 3 in–13 ft 1 in) were located between Shurgil and Kuhneh Shahr. Substantial vertical movement of the west-northwest trending fault was also seen, with even greater maximum displacements of 4–6 meters (13–20 ft), but the average vertical slip was about 1.2 meters (3 ft 11 in) throughout the extent of the observed surface faulting. Seismologists estimated that about 30 kilometers (19 mi) of visible fault breaks were present immediately following the shocks, but by the time they had completed their survey forty-five 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.[4]


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. Shikaryazi 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.[4]

See also[edit]


  1. ^ a b c d ISC (19 January 2015), ISC-GEM Global Instrumental Earthquake Catalogue (1900-2009), Version 2.0, International Seismological Centre 
  2. ^ a b c USGS (September 4, 2009), PAGER-CAT Earthquake Catalog, Version 2008_06.1, United States Geological Survey 
  3. ^ a b c d Tchalenko & Berberian 1974, pp. 151–155, 159
  4. ^ a b c Ambraseys, N.N.; Melville, C.P. (2005). A History of Persian Earthquakes. Cambridge University Press. pp. 80, 81. ISBN 0-521-02187-1. 
  5. ^ a b Tchalenko & Berberian 1974, pp. 161, 172–186, 209, 210