1991 Racha earthquake

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1991 Racha earthquake
Relief Map of Georgia.png
Bullseye1.png
UTC  time1991-04-29 09:12:48
ISC  event 336954
USGS-ANSS ComCat
Local date29 April 1991 (1991-04-29)
Local time13:13
Magnitude7.0 Mw
Depth17 km [1]
Epicenter 42°27′11″N43°40′23″E / 42.453°N 43.673°E / 42.453; 43.673
TypeBlind thrust [2]
Areas affectedFlag of Georgia (1990-2004).svg  Georgia
Max. intensity MMI IX (Violent) [3]

MSK-64 IX (Destructive)
Casualties270 dead

The 1991 Racha earthquake occurred in the province of Racha, Georgia, at 9:12 UTC on 29 April. Centered on the districts of Oni and Ambrolauri on the southern foothills of the Greater Caucasus mountains, it killed 270, left approximately 100,000 homeless and caused severe damage, including to several medieval monuments. [4] It had a magnitude of 7.0 and was the most powerful earthquake recorded in the Caucasus. [5]

Contents

Tectonic setting

Georgia lies between the two mountain chains of the Greater Caucasus in the north and the Lesser Caucasus in the south. These two sets of mountains have both resulted from the continuing effects of the collision between the Arabian Plate and the Eurasian Plate. The Greater Caucasus consists of a southward-directed fold and thrust belt that has been active since the Oligocene. Racha lies close to the southern margin of this thrust belt and the earthquake is interpreted to be caused by rupture of the active thrust front. [6]

Damage

USGS shake map for the earthquake 1991 Racha intensity.jpg
USGS shake map for the earthquake

The earthquake affected 700 villages and settlements, destroying 46,000 houses and making 100,000 people homeless. The number of casualties was reduced because most of the inhabitants were working in the fields at the time of the earthquake, 13:13 local time. Many important historical monuments were badly damaged, particularly the Archangel Church near Zemo Krikhi and the Mravaldzali church, which were completely destroyed. [4] [7]

Much of the damage associated with the earthquake was caused by landslides triggered by the shaking, rather than the shaking itself. The most common type were rock falls, followed by debris slides, slumps, earth slides, rock-block slides and rock avalanches. The most destructive was a large debris avalanche, which destroyed the village of Khokheti, killing 50 of the inhabitants. A large mass of Jurassic volcanic rock fell onto water-saturated alluvium, combining to form the debris avalanche. The debris avalanche, which had an estimated volume of over 3 million m3, swept down a valley through Khokheti, blocking the Gebura River, forming a 100-m-high dam, that breached soon afterwards, causing more destruction. Two of the earth slides showed a delayed movement, with most displacement occurring a few days after the main shock. The Chordi landslide was active before the earthquake and showed only minor movement at the time of the main shock. Two to three days later, the slide started to move at about 8 m per day, destroying the village of Chordi. On 18 May, the slide was still moving at 2 m per day. This slide moved on claystone of the Maikop Formation and had a total volume of about 20 million m3. [8]

The large aftershock on 15 June caused extensive damage in the Java to Tskhinvali area. At least 8 people were killed and 200 injured. However, due to a protest rally by the local people, dozens, but not hundreds, were killed. The village of Khakhet was destroyed. [9]

Characteristics

The earthquake had a magnitude of 7.0. A maximum intensity of IX on the MSK scale was observed. The calculated focal mechanism showed that the earthquake was a result of low-angle reverse faulting on a fault plane dipping at about 35° to the north-northeast. This was confirmed from the distribution of aftershocks, which defined a clear plane of this orientation. Analysis of the detailed velocity structure around the rupture zone suggested that it coincided with a marked change in seismic velocity, consistent with it representing the interface between Mesozoic sediments and the underlying crystalline basement. [5] The 1,500-m-high Racha Ridge is thought to have been uplifted by repeated earthquakes of this type. [6]

The mainshock was followed by a complex series of aftershocks extending over several months, which caused further damage and casualties The largest of the aftershocks, which consisted of two events about two seconds apart, had a magnitude of Ms 6.5 and occurred on 15 June with an epicenter near Java. [10] On 23 October 1992, a magnitude 6.7 earthquake occurred about 100 km east of the aftershock zone. It was also due to reverse faulting on a north-northeast-dipping plane, although with a significant dextral (right lateral) strike-slip component. [6]

Aftermath

The ongoing Georgian–Ossetian conflict complicated the rescue effort. [11]

See also

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References

  1. ↑ NGDC. "Comments for the Significant Earthquake" . Retrieved 10 August 2010.
  2. ↑ Yeats, R. S.; Sieh, K. E.; Allen, C. R. (1997). The Geology of Earthquakes. Oxford University Press. p. 363. ISBN   978-0-19-507827-5.
  3. ↑ National Geophysical Data Center / World Data Service (NGDC/WDS) (1972). "Significant Earthquake Database" (Data Set). National Geophysical Data Center, NOAA. doi:10.7289/V5TD9V7K.{{cite journal}}: Cite journal requires |journal= (help)
  4. 1 2 Nikoleishvili, I. "Earthquake in Racha and Middle Age Monuments". Archived from the original on 21 July 2011. Retrieved 10 August 2010.
  5. 1 2 Arafiev, S.S.; Rogozhin E.A.; Bykova V.V. & Dorbath C. (2006). "Deep Structure of the Racha Earthquake Source Zone from Seismic Tomography Data" (PDF). Izvestiya, Physics of the Solid Earth. 42 (1): 27–40. Bibcode:2006IzPSE..42...27A. doi:10.1134/s1069351306010034. S2CID   128784815. Archived from the original (PDF) on 7 August 2011.
  6. 1 2 3 Triep, E.G.; Abers G.A.; Lerner-Lahm A.L.; Mishatkin V.; Zakharchenko N. & Starovoit O. (1995). "Active thrust front of the Greater Caucasus: The April 29, 1991, Racha earthquake sequence and its tectonic implications" (PDF). Journal of Geophysical Research. 100 (B3): 4011–4033. Bibcode:1995JGR...100.4011T. doi:10.1029/94JB02597. Archived from the original (PDF) on 22 June 2011. Retrieved 10 August 2010.
  7. ↑ Zaalishvili, V.; Sulberidze, O.; Chelidze, T.; Varazanashvili O. & Javakhishvili Z. (2000). "Seismicity and cultural monuments of Georgia". In Balassanian S.; Cisternas A. & Melkumyan M. (eds.). Earthquake hazard and seismic risk reduction. Advances in natural and technological hazards research. Vol. 12. pp. 127–136. ISBN   978-0-7923-6390-3.
  8. ↑ Jibson, R.W.; Prentice C.S.; Borissoff B.A.; Rogozhin E.A. & Langer C.J. (1994). "Some Observations of Landslides Triggered by the 29 April 1991 Racha Earthquake, Republic of Georgia" (PDF). Bulletin of the Seismological Society of America. 84 (4). Archived from the original (PDF) on 31 May 2010. Retrieved 10 August 2010.
  9. ↑ "История конфликта в Южной Осетии. Обсуждение на LiveInternet – Российский Сервис Онлайн-Дневников".
  10. ↑ USGS (5 January 2010). "Significant Earthquakes of the World 1991". Archived from the original on 16 January 2009. Retrieved 10 August 2010.
  11. ↑ "1991–1999". Archived from the original on 21 May 2009. Retrieved 20 September 2009.
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