1963 Marj Earthquake
Tectonic setting
The northern part of Cyrenaica lies close to the northern edge of the African plate. Offshore lies the Mediterranean Ridge, an accretionary wedge, developed above the destructive plate boundary where the African plate is being subducted beneath the Aegean Sea plate along the Hellenic subduction zone. The Cyrenaica promontory is thought to be undergoing incipient collision as the continental margin enters the subduction zone. The Cyrenaica region is characterised by relatively low magnitude earthquakes with thrust fault focal mechanisms, developed in an area of NE–SW directed maximum horizontal stress.
Earthquake
The earthquake's epicenter was located about 13 km to the north-northeast of the city of Marj in the Marj District of Cyrenaica. It was felt as far away as Benghazi, about 100 km from the epicenter. The magnitude has been calculated as Mw 5.6 by the ISC. It was followed later that day by two aftershocks of over Mw 4.0.
Damage
The main area of damage was restricted to a 20 km long section of the alluvial plain around Marj, which is located between two escarpments, possibly fault-related. The maximum damage was observed at Maddalena, a village about 12 km from Marj and close to the epicenter, in which all the farmhouses collapsed. The effects of the shaking depended on the construction type of the buildings. Those built of rubble masonry were most affected, with many collapsing and causing most of the casualties. Buildings constructed from hollow concrete blocks were only moderately affected and those built with reinforced concrete were almost completely unaffected.
Aftermath
The Libyan authorities followed the recommendations of the UNESCO report and rebuilt Marj on firmer ground about 4 km away from its original location.
See also
References
- ^ ISC (2016), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2013), Version 4.0, International Seismological Centre
- ^ National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Information (Data Set), National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K
- ^ PAGER-CAT Earthquake Catalog, Version 2008_06.1, United States Geological Survey, September 4, 2009
- ^ Ambraseys, N. N.; Melville, C. P.; Adams, R. D. (2005), The Seismicity of Egypt, Arabia and the Red Sea: A Historical Review, Cambridge University Press, pp. 90, 91, ISBN 978-0521020251
- ^ Polonia, A.; Camerlenghi, A.; Davey, F.; Storti, F. (2002). "Accretion, structural style and syn-contractional sedimentation in the Eastern Mediterranean Sea". Marine Geology. 186 (1–2): 127–144. Bibcode:2002MGeol.186..127P. doi:10.1016/S0025-3227(02)00176-7.
- ^ Capitanio, F.A.; Faccena, C.; Funiciello, R.; Salvini, F. (2011). "Recent tectonics of Tripolitania, Libya: an intraplate record of Mediterranean subduction". In Van Hinsbergen, D.J.J.; Buiter, S.J.H.; Torsvik, T.H.; Gaina, C.; Webb, S.J. (eds.). The Formation and Evolution of Africa: A Synopsis of 3.8 Ga of Earth History. Special Publications. Vol. 357. Geological Society, London. doi:10.1144/SP357.17. ISBN 978-1-86239-335-6. S2CID 131721574.
- ^ Al-Heety, E. (2013). "Seismicity and seismotectonics of Libya: as an example of intraplate environment". Arabian Journal of Geosciences. 6 (1): 193–204. Bibcode:2013ArJG....6..193A. doi:10.1007/s12517-011-0347-y. S2CID 129425103.
- ^ Minami, K. (1963). Relocation and reconstruction of the Town of Barce,Cyrenaica, Libya, damaged by the earthquake of 21 February 1963 (PDF) (Report). UNESCO.
- ^ Cousins, M. (November 12, 2017). "Small earthquake in Marj, no one hurt". LibyaHerald. Retrieved July 1, 2022.
External links
- M 5.6 – near the coast of Libya – United States Geological Survey
- The International Seismological Centre has a bibliography and/or authoritative data for this event.