The 2011 Lorca earthquake was a moderate 5.1 earthquake that occurred 6:47 p.m. CEST on 11 May 2011, near the town of Lorca, causing significant localized damage in the Region of Murcia, Spain, and panic among locals, and displacing many from their homes. The quake was preceded by a magnitude 4.4 foreshock at 17:05, that inflicted substantial damage to many older structures in the area, including the historical Espolón Tower of Lorca Castle, the Hermitage of San Clemente and the Convent of Virgen de Las Huertas. Three people were killed by a falling cornice. A total of nine deaths have been confirmed, while dozens are reported injured. The earthquake was the worst to hit the region since a 5.0 Mw tremor struck west of Albolote, Granada in 1956.
Geology
The magnitude 5.1 main shock occurred inland on 11 May 2011 at 18:47 local time in the locality of Lorca, Spain, at a depth of. Much of the southern Iberian Peninsula – in particular the Murcia Region – is located on a tectonic zone of common seismic activity, where a plate boundary separating the Eurasia and African Plates is formed. However, most tremors in the region do not exceed perceptible magnitudes. The earthquake was estimated to be a direct result of strike-slip faulting near the major , along an unusually shallow fault of between 40 and 50 km long. Local specialists also reported the presence of surface rupturing in the vicinity of the fault. Due to the shallow depth, the earthquake resulted in significant shaking throughout much of Murcia. In Lorca, near the epicentre of the quake, strong ground motions registered a maximum intensity of VI on the Mercalli scale, while many adjacent areas reported moderate shaking. Widespread light tremors were observed in locations up to several hundred kilometers from the epicentre, including Alicante and Madrid.
Foreshock
The earthquake was preceded by a magnitude 4.5 foreshock that struck very close to its epicentre at 17:05 local time. It was reported to be centred along the same fault zone, with a similar focal mechanism as the main shock. Though the tremor was relatively mild, some cracks and crumbled walls were reported, while downed power lines sparked a small fire in Lorca.
Aftershock
As of 11 May, at least eight light aftershocks were reported near the initial quake epicentres; the strongest registered a magnitude of 4.1 and occurred at 22:37 local time.
Emergency management
Shortly after the second earthquake struck, the Spanish government, at the request of regional government of Murcia, activated the Military Emergencies Unit, a branch of the Spanish Armed Forces responsible for providing disaster relief. 340 members from three battalions were dispatched to Lorca under the management of the Lieutenant Colonel of the Bétera battalion; these were later joined by army units. A field hospital was set up by the Military Emergencies Unit in the Plaza del Ayuntamiento where those injured were attended to by members of Protección Civil and the Red Cross. earthquake epicentre zones with damaged buildings deaths
Possible causes
Several research groups investigated the cause of this earthquake. The Active Tectonics Group of the Complutense University of Madrid in collaboration with the :es:Instituto Andaluz de Geofísica y Prevención de Desastres Sísmicos|Instituto Andaluz de Geofísica using tectonic evidences, InSAR analysis and seismological analysis of the rupture concluded that this earthquake was produced by the reactivation of a small section of the Alhama de Murcia Fault located 3 km northeast of Lorca, Spain. These conclusions were published in the journal Tectonophysics in April 2012. The great damage produced by this moderate magnitude earthquake may be explained by the southwestward directivity of a shallow rupture that induced high acceleration values in Lorca village. From the tectonic point of view this earthquake can be considered as an ordinary event coherent with the tectonic evolution and mechanical characteristics of the Alhama de Murcia Fault. In fact, similar earthquakes occurred in Lorca in the 16th and 17th centuries. Several research projects conducted during the last 25 years on this fault recognized the occurrence of much larger earthquakes during the last 10,000 years. Other scientific research has suggested that the earthquake was caused by human activity. A team led by Dr Pablo Gonzalez of the University of Western Ontario in Canada reported in the journal Nature Geoscience in October 2012 that the pattern of earth movement was consistent with changes in stresses caused by the removal of water from underground reservoirs.
