Reappraisal of the 1863 Huércal-Overa Earthquake (Betic Cordillera, SE Spain) by the Analysis of ESI-07 Environmental Effects and Building Oriented Damage

• Published in: Geosciences (Basel) 2020-08, Vol.10 (8), p.303
• Main Authors: Silva, Pablo G., Elez, Javier, Giner-Robles, Jorge L., Pérez-López, Raúl, Roquero, Elvira, Rodríguez-Pascua, Miguel Ángel
• Format: Article
• Language: English
• Subjects: Aftershocks; Anomalies; Betic Cordillera; Building damage; Cracking (fracturing); Cultural heritage; Damage detection; Data; Diagnostic systems; Earth science; Earthquake Archaeological Effects (EAEs); Earthquake damage; Earthquake Environmental Effects (EEEs); Earthquakes; Engineers; Environmental effects; ESI-07 Intensity Scale; Geology; Hydrogeology; Lakes; Religious buildings; SE Spain; Seismic activity; Shaking; Spatial distribution
• ISSN: 2076-3263; 2076-3263
• DOI: 10.3390/geosciences10080303

This work reviews the 1863 Huércal-Overa earthquake (VI-VII EMS) based on the environmental seismic intensity scale (ESI-07) and oriented archaeoseismological building damage. The performed analysis identifies 23 environmental effects (EEEs) and 11 archaeoseismological effects (EAEs), completing a total of 34 intensity data-points within the intensity zone ≥ VI EMS. The new ESI intensity data quintuplicate the previous intensity data-points ≥ VI EMS (five localities) for this event. Sixteen of the identified EEEs indicate the occurrence of intensity VII-VIII within the Almanzora valley, south of Huércal-Overa, over an area of ca. 12–15 km2. Anomalies in water bodies, slope movements, hydrogeological anomalies, ground cracking, and other effects (gas emissions, tree shaking) are the more diagnostic EEEs—with one of them indicating a local maximum intensity of VIII-IX ESI-07 (Alboraija lake). Environmental earthquake damage of intensity ≥ VI covers an area of c. 100 km2, compatible with a VIII ESI intensity event. The spatial distribution of EEEs and EAEs indicates that the zone of Almanzora River Gorge, which was depopulated during the earthquake epoch, was the epicentral area, and compatible with seismotectonic data from active shallow blind thrusting beneath the Almagro Range. The use of ESI data in nearly unpopulated areas help to fill gaps between damaged localities (EMS data) multiplying intensity data-points, providing a better definition of the intensity zones and offering a geological basis to look for suspect seismic sources.