1931 Zangezur earthquake

1931 Zangezur earthquake
Date April 27, 1931
Magnitude Ms 6.3
Depth 22 km
Epicenter 39°12′N 46°00′E / 39.20°N 46.00°ECoordinates: 39°12′N 46°00′E / 39.20°N 46.00°E
Areas affected Armenia
Azerbaijan
Max. intensity MSK – IX (Destructive)
Casualties 2,890 deaths

The 1931 Zangezur earthquake occurred on April 27 at 16:50 UTC with an estimated magnitude of Ms 6.3 or Ms 6.5, according to different sources.[1][2] The earthquake was located in the Zangezur Mountains near the boundary between southwestern Armenia and Azerbaijan's exclave, the Nakhichivan Autonomous Republic. Both territories were part of the Soviet Union at that time.[1]

The earthquake was located near the border between the Syunik Province of Armenia (Zangezur is an alternative name for the region of Syunik Province) and the Nakhichivan Autonomous Republic of Azerbaijan. The number of reported dead in the earthquake was 2,890.[1] In Armenia, 57 villages were destroyed or heavily damaged in the Sisian-Goris area and in Azerbaijan, 46 villages were destroyed or seriously damaged in the Ordubad area.[3] In another source it was reported that the earthquake destroyed 254 villages.[4] In southeastern Armenia, the historical Tatev Monastery was damaged. The intensities reached MSK-64 IX in Shamb and MSK-64 VIII in Jougha.[5] The Museum of History in Sisian has some photos taken after the town was hit by the earthquake.[6]

The Pambak-Sevan-Sunik Fault extends in the NW-SE direction. The fault can be traced continuously for 400 km and consists of four major segments. The 1931 Zangezur earthquake was located in the area of the Sunik-Zanghezour segment, which is about 120 km long.[7]

There was a period of increased earthquake activity in Armenia and its neighboring republics between 1911 and 1956 and the 1931 event was one of the strongest. It released about half of the total energy of all the earthquakes occurring in the Caucasus region near the Caspian Sea in that period.[8]

See also

References

  1. ↑ 1.0 1.1 1.2 National Geophysical Data Center / World Data Service (NGDC/WDS) Significant Earthquake Database, Boulder, CO, USA. (Available at http://www.ngdc.noaa.gov/nndc/struts/form?t=101650&s=1&d=1)
  2. ↑ "STATISTICAL PREDICTION OF THE SEQUENCE OF LARGE EARTHQUAKES IN IRAN" by A. Yazdani and M. Kowsari
  3. ↑ http://earthquake.usgs.gov/learn/today/index.php?month=4&day=27&submit=View+Date
  4. ↑ http://gsi.ir/General/Lang_en/Page_29/TypeId_/DataId_128/Action_Pn4/WebsiteId_13/Twentieth.Century.Seismicity.of.Maku.Region. (1900.1977).html
  5. ↑ "Evidence of historical seismicity and volcanism in the Armenian Highland (from Armenian and other sources)" by A. Karakhanian and Y. Abgaryan
  6. ↑ "Georgia, Armenia & Azerbaijan" by J. Noble, M. Kohn, and D. Systermans. Lonely Planet. 2008.
  7. ↑ Philip, Hervé; Avagyana, Ara; Karakhanian, Arcadi; Ritz, Jean-François; Rebai, Samira (2001). "Estimating slip rate and recurrence intervals for strong earthquakes along an intracontinental fault: example of the Pambak-Sevan-Sunik fault (Armenia)". Tectonophysics (Elsevier) 343 (3-4): 206–232. Bibcode:2001Tectp.343..205P. doi:10.1016/S0040-1951(01)00258-X.
  8. ↑ "ON THE PERIODICITY OF SEISMIC ACTIVITY DURING THE LAST ONE AND A HALF TO TWO THOUSAND YEARS (BASED ON THE EXAMPLE OF ARMENIA)" by G. P. Tamrazyan