1968 Dasht-e Bayaz and Ferdows earthquakes
   Tehran | |
| UTC time | 1968-08-31 10:47:43 |
|---|---|
| ISC event | 818488 |
| USGS-ANSS | ComCat |
| Local date | August 31, 1968 |
| Local time | 14:17:43 |
| Duration | 1–2 minutes [1] |
| Magnitude | 7.1 Mw[2] |
| Epicenter | 34°01′N 58°58′E / 34.02°N 58.96°E |
| Areas affected | Iran |
| Max. intensity | X (Extreme) [1] |
| Aftershocks | 6.4 Mw Sept 1 at 07:27 [3] |
| Casualties | 15,000 August 31 [4] 900 September 1 [4] |
The Dasht-e Bayaz and Ferdows earthquakes occurred in Dashte Bayaz, Kakhk and Ferdows, Iran in late August and early September 1968. The mainshock measured 7.4 on the moment magnitude scale and had a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. Damage was heavy in the affected areas with thousands of lives lost in the first event and many hundreds more in the second strong event.
Tectonic setting
The Iranian plateau is confined by the Turan platform in the north and the Zagros fold and thrust belt and Makran Trench in the south. The Arabian Plate is converging to the north with the Eurasian Plate at a rate of 35 millimeters (1.4 in) per year, and is diffused across a 1,000 km (620 mi) zone resulting in continental shortening and thickening throughout the plateau, with strike-slip and reverse faulting present, as well as subduction at the Makran coast.[5]
In eastern Iran, the shortening is accommodate by a combination of relatively short northwest–southeast trending reverse faults, long north–south trending right lateral strike-slip faults and shorter west–east trending left-lateral strike-slip faults.[2]
Earthquakes
The first earthquake occurred on August 31, 1968, measuring 7.1 on the moment magnitude scale. The focal mechanism indicated strike-slip faulting and the observed 80 km surface rupture showed that this earthquake resulted from movement on the western part of the west–east trending left-lateral Dasht-e-Bayaz Fault. The greatest observed left-lateral coseismic offset was about 4.5 m, with 2 m being the average observed offset.[2]
Damage
The mainshock destroyed five villages in the Dasht-e Bayaz area, and at least half of the buildings in another six villages from Kakhk to Sarayan. A strong aftershock on September 1, measuring 6.4 on the moment magnitude scale, destroyed Ferdows. More than 175 villages were destroyed or damaged in this earthquake.
See also
References
- ^ a b Niazi, M. (1969), "Source dynamics of the Dasht-e Bayāz earthquake of August 31, 1968", Bulletin of the Seismological Society of America, 59 (5): 1857, 1859
- ^ a b c Walker, R.; Jackson, J.; Baker, C. (2004). "Active faulting and seismicity of the Dasht-e-Bayaz region, eastern Iran". Geophysical Journal International. 157 (1): 265–282. doi:10.1111/j.1365-2966.2004.02179.x.
- ^ Ambraseys, N. N.; Melville, C. P. (1982), A History of Persian Earthquakes, Cambridge Earth Science Series, Cambridge University Press, p. 165, ISBN 978-0521021876
- ^ a b Utsu, T. R. (2002), "A List of Deadly Earthquakes in the World: 1500–2000", International Handbook of Earthquake & Engineering Seismology, Part A, Volume 81A (First ed.), Academic Press, p. 707, ISBN 978-0124406520
- ^ Berberian, M.; Yeats, R. (1999), "Patterns of historical earthquake rupture in the Iranian Plateau", Bulletin of the Seismological Society of America, 89 (1): 120
Further reading
- Ambraseys, N.; Tchalenko, J. S. (1969), "The Dasht-e Bayāz (Iran) earthquake of August 31, 1968: A field report", Bulletin of the Seismological Society of America, 59 (5): 1751–1792
- Crampin, S. (1969), "Aftershocks of the Dasht-e Bayāz, Iran, earthquake of August, 1968", Bulletin of the Seismological Society of America, 59 (5): 1823–1841
External links
- Earthquakes with 1,000 or More Deaths since 1900 – United States Geological Survey
- The International Seismological Centre has a bibliography and/or authoritative data for this event.
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