1968 Dasht-e Bayaz and Ferdows earthquakes

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1968 Dasht-e Bayaz and Ferdows earthquakes
1968 Dasht-e Bayaz and Ferdows earthquakes is located in Iran
1968 Dasht-e Bayaz and Ferdows earthquakes
Tehran
Tehran
UTC time1968-08-31 10:47:43
ISC event818488
USGS-ANSSComCat
Local dateAugust 31, 1968 (1968-08-31)
Local time14:17:43
Duration1–2 minutes [1]
Magnitude7.1 Mw[2]
Epicenter34°01′N 58°58′E / 34.02°N 58.96°E / 34.02; 58.96
Areas affectedIran
Max. intensityMMI X (Extreme) [1]
Aftershocks6.4 Mw Sept 1 at 07:27 [3]
Casualties15,000 August 31 [4]
900 September 1 [4]

The Dasht-e Bayaz and Ferdows earthquakes (Persian: زمین‌لرزه ۱۳۴۷ دشت بیاض و زمین لرزه فردوس) 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

See also: Alborz and Caspian Depression

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

USGS Shakemap for the August 31 event

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] The western end of the Dasht-e-Bayaz Fault ruptured and produced another large earthquake in 1979.[6]

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

  1. ^
    doi:10.1785/BSSA0590051843[permanent dead link
    ]
  2. ^
    doi:10.1111/j.1365-2966.2004.02179.x
    .
  3. ISBN 978-0521021876
  4. ^
    ISBN 978-0124406520
  5. doi:10.1785/BSSA0890010120, archived from the original
    on January 10, 2012
  6. doi:10.1111/j.1365-246X.2011.05213.x.{{cite journal}}: CS1 maint: multiple names: authors list (link
    )

Further reading

External links


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