1968 Belice earthquake

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1968 Belice earthquake
Relief map of Italy Sicily.png
Bullseye1.png
UTC  time1968-01-15 02:01:06
ISC  event 827285
USGS-ANSS ComCat
Local date14 January 1968 (1968-01-14) [1]
Local time03:01
Magnitude5.5 Mw [2]
Epicenter 37°46′01″N12°58′59″E / 37.767°N 12.983°E / 37.767; 12.983 [3]
Type Thrust
Areas affected Sicily
Max. intensity X (Extreme)
Casualties231–400 dead
632–1,000 injured

The 1968 Belice earthquake sequence took place in Sicily between 14 and 15 January. [3] The largest shock measured 5.5 on the moment magnitude scale, with five others of magnitude 5+. [2] The maximum perceived intensity was X (Extreme) on the Mercalli intensity scale. The earthquake sequence, centred between the towns of Gibellina, Salaparuta and Poggioreale, killed at least 231 people, possibly more than 400, with between 632 and about 1,000 injured and left 100,000 homeless. It is known in Italy as Terremoto del Belice.

Contents

Tectonic setting

Sicily lies on the complex convergent plate boundary between the African Plate and the Eurasian Plate. The geology of the western part of the island is dominated by the Gela Nappe, a thin-skinned fold and thrust belt. The Gela Nappe consists of Pliocene-Quaternary age sedimentary rocks deposited in the earlier foredeep, thrust up onto the thick carbonate sequence of the Pelagian-Hyblean Platform of the African Plate. [2]

Earthquake

There was a sequence of six M 5+ earthquakes, making this western Sicily's largest historical seismic event, [1] beginning with a M 5.2 shock at 12:28 on the 14 January, followed by a M 5.1 event at 13:15 on the same day and a M 5.2 event at 01:33 on 15 January, the mainshock at 02:01, and two M 5.2 events at 16:42 on 16 January and at 09:56 on 25 January. [2]

The greatest perceived intensity on the Mercalli scale was X (Extreme) at Gibellina, Montevago and Salaparuta. Intensities at Poggioreale, Santa Margherita di Belice, Santa Ninfa, Partanna and Salemi reached IX (Violent) on the scale. [3]

The ruins of Poggioreale pictured in 2003 Poggioreale ruderi2.jpg
The ruins of Poggioreale pictured in 2003

The focal mechanisms of the mainshock and the two magnitude 5+ aftershocks are consistent with thrusting on faults trending west–east, [1] although an alternative solution has been proposed for the mainshock of right lateral transpression on a NNW-SSE trending fault. [2]

Damage

The main area of damage was centred on the valley of the Belice, with worst affected towns being Santa Ninfa, Partanna, Montevago, Santa Margherita di Belice, Gibellina, Salaparuta, Poggioreale. [4] : 8  Vita, Salemi, and Camporeale also suffered significant damage. [4] : 2 

The earthquakes on 14 January did little damage, but many of the inhabitants spent the following night sleeping outside, during which the most damaging of the shocks occurred, [5] which probably greatly reduced the number of casualties. [3] The official death toll was 231 with a further 623 injured. Other estimates give more than 400 dead with over 1,000 injured. An estimated 100,000 people were made homeless by the earthquakes. [3]

The worst affected buildings were of unreinforced masonry construction that used irregular stones with weak mortar and had roofs consisting of heavy tiles resting on wooden beams. Such buildings collapsed completely in many cases. Houses with load-bearing walls made of regular stone or concrete blocks and better quality mortar performed better, although some were badly damaged. The most modern buildings that used reinforced concrete frames generally suffered little damage. [4] : 10 

Aftermath

Abandoned buildings in Poggioreale, 2007 Poggioreale 2007.jpg
Abandoned buildings in Poggioreale, 2007

The immediate relief effort was hampered by a lack of disaster relief planning at both local and provincial levels, excessive bureaucracy, a lack of supplies close to the affected areas and a tendency of refugees to treat outsiders with suspicion. [4] : 59 

One year after the earthquakes, many hundreds of people were still living in tents and many of the prefabricated housing units had yet to appear, despite having been paid for; no work had begun on providing permanent housing. Two-thirds of refugee families had still not received their government grant. [4] : 52  Nine years after the earthquake, none of the refugees had been placed in new housing, leaving 60,000 still living in temporary accommodation. [6]

The towns of Poggioreale, Gibellina, Vita, Santa Margherita di Belice and Salaparuta were eventually rebuilt in new locations. [3]

See also

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References

  1. 1 2 3 Monaco, C.; Mazzoli S.; Tortorici L. (1996). "Active thrust tectonics in western Sicily (southern Italy): the 1968 Belice earthquake sequence". Terra Nova. 8 (4): 372–381. Bibcode:1996TeNov...8..372M. doi:10.1111/j.1365-3121.1996.tb00570.x.
  2. 1 2 3 4 5 Lavecchia, G.; Ferrarini F.; de Nardis R.; Visini F.; Barbano M.S. (2007). "Active thrusting as a possible seismogenic source in Sicily (Southern Italy): Some insights from integrated structural–kinematic and seismological data". Tectonophysics. 445 (3–4): 145–167. Bibcode:2007Tectp.445..145L. doi:10.1016/j.tecto.2007.07.007.
  3. 1 2 3 4 5 6 Guidoboni, E.; Ferrari G.; Mariotti D.; Comastri A.; Tarabusi G.; Valensise G. "Catalogue of Strong Earthquakes in Italy (461 BC – 1997) and Mediterranean Area (760 B.C. – 1500)". INGV-SGA. Retrieved 8 May 2019.
  4. 1 2 3 4 5 Haas, J. Eugene; Robert S. Ayre (1969). The Western Sicily Earthquake Of 1968. Washington, D.C.: National Academy of Sciences. Retrieved July 11, 2011.
  5. ↑ The Civil Protection Department (Protezione Civile). "Belice earthquake 1968". Archived from the original on 7 April 2012. Retrieved 1 July 2012.
  6. ↑ Ginsborg, P. (2003). A History of Contemporary Italy: Society and Politics, 1943–1988. Palgrave Macmillan. pp. 345–346. ISBN   978-1-4039-6153-2 . Retrieved 1 July 2012.

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