Abstract
One of the most destructive historical earthquakes (M ≈6.7) in Spain occurred in 1884 along the normal Ventas de Zafarraya Fault located in the Central Betic Cordilleras. Palaeoseismic and radiocarbon data presented in this study are the first to constrain the timing of the pre-1884 fault history in the last 10 ka. These data yield a recurrence interval of between 2 and 3 ka for major earthquakes, under the assumption of uniform return periods along the normal fault. The Holocene slip rate is estimated to be in the order of 0.35±0.05 mm/year, which is significantly higher than the mean slip rate of 0.17±0.03 mm/year since the Tortonian. Several of the most important deformations and secondary features, such as landslides and liquefaction, are related to strong ground motion and document the Holocene activity of the Ventas de Zafarraya Fault.
Similar content being viewed by others
References
Alfaro P, Galindo-Zaldívar J, Jabaloy A, López-Garrido AC, Sanz de Galdeano C (2001) Evidence for the activity and paleoseismicity of the Padul fault (Betic Cordillera, southern Spain). Acta Geol Hisp 36:283–295
Basson U, Enzel Y, Amit R, Ben-Avraham Z (1994) Detecting and mapping recent faults with a ground penetrating radar in the alluvial fans of the Arava valley, Israel. In: Proc 5th Conference on Ground Water Penetrating Radar. Waterloo Centre for Groundwater Research; Kitchener, Ontario, pp 777–788
Bell JW, Amelung F, King GCP (1997) Preliminary Late Quaternary slip history of the Carboneras Fault, southeastern Spain. J Geodynamics 24:51–66
Buforn E, Udias A, Colombas MA (1988) Seismicity, source mechanisms and tectonics of the Azores–Gibraltar plate boundary. Tectonophysics 152:89–118
Cai J, McMechan GA, Fisher MA (1996) Application of ground-penetrating radar to investigation of near-surface fault properties in the San Francisco Bay region. Bull Seism Soc Am 86:1459–1470
DeMets C, Gordon RG, Argus DF, Stein S (1990) Current plate motions. Geophys J Int 101:425–478
Douvillé R (1906) La Péninsule Iberíque. III(3):pp 1–175
Fernández-Fernández E, Campos J, González-Lodeiro F (1992) Estructuras extensionales en las rocas alpujárrides al E de Málaga (Sierra Tejeda, Cordilleras Béticas). Geogaceta 12:13–16
Galindo-Zaldívar J, González-Lodeiro F, Jabaloy A (1993) Stress and palaeostress in the Betic-Rif cordilleras (Miocene to the present). Tectonophysics 227:105–126
Galindo-Zaldívar J, Jabaloy A, Serrano I, Morales J, González-Lodeiro F, Torcal F (1999) Recent and present-day stresses in the Granada Basin (Betic Cordilleras): example of a late Miocene–present-day extensional basin in a convergent plate boundary. Tectonics 18:686–702
Galindo-Zaldívar J, Ruano P, Jabaloy A, López-Chicano M (2000) Kinematics of faults between Subbetic Units during the Miocene (central sector of the Betic Cordillera). CR Acad Sci Paris 331:811–816
Galindo-Zaldívar J, Gil AJ, Borque MJ, González-Lodeiro F, Marín-Lechado C, Jabaloy A, Ruano P, Sanz de Galdeano C (2003) Active faulting in the internal zones of the central Betic Cordillera (SE Spain). J Geodynam 36:239–250
García-Hernández M, Lopez-Garrido AC, Rivas P, Sanz de Galdeano C, Vera JA (1980) Mesozoic palaeogeographic evolution of the external zones of the Betic Cordillera. Geol Mijnb 59:155–168
Herraiz M, De Vicente G, Lindo-Ñaupari R, Giner J, Simón JL, González-Casado JM, Vadillo O, Rodríguez-Pascua MA, Cicuéndez JI, Casas A, Cabañas L, Rincón P, Cortés AL, Ramírez M, Lucini M (2000) The recent (upper Miocene to Quaternary) and present tectonic stress distributions in the Iberian Peninsula. Tectonics 19:762–786
Ibañez JM, Bottari C, Esquivel JA, Morales J, Alguacil AG (2003) Magnitude-intensity relations for instrumental and historical (IX–XIX century) earthquakes in south Spain. Tectonical and seismic hazard implications. Bull Seism Soc Am ( in press)
Keefer DK (1984) Landslides caused by earthquakes. Geol Soc Am Bull 95:406–421
Kilian W (1889) Mission d’ Andalousie. Mem Ac Soc 30:1–582
Lonergan L, Platt JP, Gallagher L (1994) The internal–external zone boundary in the eastern Betic Cordillera, SE Spain. J Struct Geol 16:175–188
López-Arroyo A, Martín-Martín AJ, Mezcua Rodríguez J (1980) Terremoto de Andalucía. Influencia en sus efectos de las condiciones del terreno y del tipo de construcción. In: Instituto Geografico Nacional (ed) El Terremoto de Andalucía del 25 de diciembre de 1884. Madrid
López-Casado C, Molina-Palacios S, Delgado J, Peláez JA (2000) Attenuation of intensity with epicentral distance in the Iberian Peninsula. Bull Seism Soc Am 90:34–47
Marco S, Agnon A, Ellenblum R, Eidelman A, Basson U, Boas A (1997) 817-year-old walls offset sinistrally 2.1 m by the Dead Sea transform, Israel. J Geodynam 24:11–20
Martínez-Díaz JJ, Masana E, Hernández-Enrile JL, Santanach P (2001) Evidence for coseismic events of recurrent prehistoric deformation along the Alhama de Murcia fault, southeastern Spain. Acta Geol Hisp 36:315–327
Martínez-Martínez JM, Anazõn JM (2002) Orthogonal extension in the hinterland of the Gibraltar Arc (Betics, SE Spain). In: Rosenbaum G, Lister GS (eds) Reconstruction of the Alpine–Himalayan orogeny. J Virtual Explorer 8 (as pdf-file)
Masana E, Santanach P (eds) (2001) Paleoseismology in Spain. Acta Geol Hisp 36
Masana E, Martínez-Díaz JJ, Hernández-Enrile JL, Santanch P (2003) The Alhama de Murcia fault (SE Spain), a seismogenic fault in a diffuse plate boundary. Seismotectonic implications in the Ibero-Maghrebian region. J Geophys Res (in press)
McCalpin JP (1996) Paleoseismology. International Geophysics Series vol 62, Academic Press, New York
Meschede M, Asprion U, Reicherter K (1997) Visualization of tectonic structures in shallow-depth high-resolution ground-penetrating radar (GPR) profiles. Terra Nova 9:167–170
Morales J, Singh SK, Ordaz M (1996) Analysis of the Granada (Spain) earthquake of 24 June, 1984 (M=5) with emphasis on seismic hazard in the Granada Basin. Tectonophysics 257:253–262
Morales J, Serrano I, Vidal F, Torcal F (1997) The depth of the earthquake activity in the Central Betics (Southern Spain). Geophys Res Lett 24:3289–3292
Muñoz M, Udias A (1980) Estudio de los Parámetros y Serie de Réplicas del Terremoto de Andalucía del 25 de Diciembre de 1884 y de la Sismicidad de la Región Málaga-Granada. In: Instituto Geografico Nacional (ed) El Terremoto de Andalucía de 1884, Madrid, pp 95–139
Muñoz M, Udias A (1982) Historical development of Spain’s catalogue of earthquakes. Bull Seism Soc Am 72:1039–1042
Ollero E, García JL (1984) Morfología del sustrato y geometría del acuífero aluvial del Polje de Zafarraya. Ist Congreso Español Geol 4:307–315
Orueta and Duarte D (1885) Informe de los terremotos ocurridos en el sur de España en diciembre de 1884 y enero de 1885. Tip Fausto Muñoz, Málaga, pp 1–51
Peláez Montilla JA, Sanz de Galdeano C, López Casado C (2001) Potencialidad sísmica de las Fallas de la Cuenca de Granada. In: Sanz de Galdeano C, Peláez Montilla JA López-Garrido AC (eds) La Cuenca de Granada. Spain, pp 158–174
Posadas AM, Vidal F, De Miguel F, Peña J, Alguacil G, Ibañez JM, Morales J (1993) Spatial–temporal analysis of a seismic swarm using the principal component analysis. The Antequera swarm (Spain), 1989. J Geophys Res 98 B2:1923–1932
Reicherter K (2001) Paleoseismological advances in the Granada Basin (Betic Cordilleras, southern Spain). Acta Geol Hisp 36(3–4):267–281 (Paleoseismology of Spain volume)
Reicherter K, Reiss S (2001) The Carboneras Fault Zone (southeastern Spain) revisited with ground penetrating radar—Quaternary structural styles from high-resolution images. Nether J Earth Sci/Geol Mijnbouw 80:129–138
Reicherter K, Jabaloy A., Galindo-Zaldívar J, Ruano P (1999) Active faults in the Granada Depression and Zafarraya areas (Betic Cordilleras). Geogaceta 27:193–196
Reiss S, Reicherter K, Reuther CD (2003) Visualization and characterization of active normal faults and associated sedimentary structures by high-resolution GPR. J Geol Soc Lond Spec Publ 211:247–255
Saccorotti G, Carmona E, Ibáñez JM, del Pezzo E (2001) Spatial characterization of Agron, southern Spain, 1988–1989 seismic series. Phys Earth Planet Interior 3983:1–17
Sandmeier KJ (2000) ReflexW version 2.1.2, user manual. Karlsruhe, Germany
Sanz de Galdeano C (1985) La fracturación del borde sur de la Depresión de Granada (discusión acerca del ecenario del terremoto del 25-XII-1884). Estud Geol 41:59–68
Serrano I (1999) Distribución espacial de la sismicidad en las Cordilleras Béticas-Mar de Alborán. PhD Thesis, University of Granada
Silva, PG, Goy JL, Zazo C, Lario J, Bardají T (1997) Paleoseismic indications along ‘aseismic’ fault segments in the Guadalentín Depression (SE Spain). J Geodynam 24:105–115
Slemmons DB, DePolo CM (1986) Evaluation of active faulting and related hazards. In: Wallace RE (ed) Active tectonics. Studies in geophysics. National Academy of Sciences, Washington, DC, pp 45–62
Stuiver M, Polach HA (1977) Discussion: reporting of 14C data. Radiocarbon 19(3):355–563
Taramelli T, Mercalli G (1886) I terrimoti andalusi cominciati il 25 dicembre 1884. Atti de la R Accad dei Lincei 83 Roma
Udías A, Muñoz D (1979) The Andalusian earthquake of 25 December 1884. Tectonophysics 53:291–297
Vidal F (1986) Sismotectónica de la región Bética-Mar de Alborán. PhD Thesis, University of Granada
Wallace RE (ed) (1986) Active tectonics. Studies in geophysics. National Academy of Sciences, Washington, DC
Wells DL, Coppersmith KL (1994) New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bull Seismol Soc Am 84:974–1002
Acknowledgements
We are thankful to both anonymous reviewers and to the associate editor for helpful and in-depth comments on the paper. The German Science Foundation, DFG-project Re 1361/3-1, and the Spanish CICYT, projects BET2000-1490-C02-01 and REN2001-3378/RIES, REN2001-2418C04-04/RIES, are thanked for financial support. 14C-dating was partly carried out at the Leibniz Labor (Univ. of Kiel).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Reicherter, K.R., Jabaloy, A., Galindo-Zaldívar, J. et al. Repeated palaeoseismic activity of the Ventas de Zafarraya fault (S Spain) and its relation with the 1884 Andalusian earthquake. Int J Earth Sci (Geol Rundsch) 92, 912–922 (2003). https://doi.org/10.1007/s00531-003-0366-3
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00531-003-0366-3