Articles | Volume 15, issue 7
https://doi.org/10.5194/se-15-837-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-15-837-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Palaeoseismic crisis in the Galera Fault (southern Spain): consequences in Bronze Age settlements?
Departamento de Ciencias de la Tierra y del Medio Ambiente, Facultad de Ciencias, Universidad de Alicante, 03080 Alicante, Spain
Ivan Medina-Cascales
Departamento de Ciencias de la Tierra y del Medio Ambiente, Facultad de Ciencias, Universidad de Alicante, 03080 Alicante, Spain
Francisco Juan García-Tortosa
Centro de Estudios Avanzados en Ciencias de la Tierra (CEACTierra), Universidad de Jaén, Campus de las Lagunillas s/n, 23071 Jaén, Spain
Departamento de Geología, Facultad de Ciencias, Universidad de Jaén, Campus Las Lagunillas s/n, 23071 Jaén, Spain
Maria Oliva Rodríguez-Ariza
Instituto Universitario de Investigación en Arqueología Ibérica, Universidad de Jaén, Campus Las Lagunillas s/n, 23071 Jaén, Spain
Fernando Molina González
Departamento de Prehistoria y Arqueología, Facultad de Filosofía y Letras, Universidad de Granada, Campus Universitario de Cartuja, 18071 Granada, Spain
Juan Antonio Cámara Serrano
Departamento de Prehistoria y Arqueología, Facultad de Filosofía y Letras, Universidad de Granada, Campus Universitario de Cartuja, 18071 Granada, Spain
Pedro Alfaro
Departamento de Ciencias de la Tierra y del Medio Ambiente, Facultad de Ciencias, Universidad de Alicante, 03080 Alicante, Spain
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P. Alfaro, J. Delgado, F. J. García-Tortosa, J. J. Giner, L. Lenti, C. López-Casado, S. Martino, and G. Scarascia Mugnozza
Nat. Hazards Earth Syst. Sci., 12, 3631–3643, https://doi.org/10.5194/nhess-12-3631-2012, https://doi.org/10.5194/nhess-12-3631-2012, 2012
Related subject area
Subject area: Tectonic plate interactions, magma genesis, and lithosphere deformation at all scales | Editorial team: Seismics, seismology, paleoseismology, geoelectrics, and electromagnetics | Discipline: Palaeoseismology
A 2600-year-long paleoseismic record for the Himalayan Main Frontal Thrust (western Bhutan)
Romain Le Roux-Mallouf, Matthieu Ferry, Rodolphe Cattin, Jean-François Ritz, Dowchu Drukpa, and Phuntsho Pelgay
Solid Earth, 11, 2359–2375, https://doi.org/10.5194/se-11-2359-2020, https://doi.org/10.5194/se-11-2359-2020, 2020
Short summary
Short summary
The chronology of historical earthquakes (from historical documents and geological evidence) is still poorly constrained in the western Himalaya. We carried out a field investigation in SW Bhutan along the India–Bhutan border. Our analysis reveals that Bhutan has experienced at least five great earthquakes during the last 2600 years. Coseismic slip values along the Main Himalayan Thrust for most events reach at least 13 m and suggest that associated magnitudes are in the range of Mw 8.5–9.
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Short summary
We investigated prehistoric earthquakes produced by the Galera Fault (southern Spain) over the last 24 000 years. From this analysis, we deduced the basic parameters that allow for the characterization of the seismic hazard of this fault. Furthermore, we discuss how the Galera Fault is prone to producing seismic crises. We also propose that one of these crises could have been responsible for the abandonment of Bronze Age human settlements located near the fault.
We investigated prehistoric earthquakes produced by the Galera Fault (southern Spain) over the...