Articles | Volume 12, issue 5
Nat. Hazards Earth Syst. Sci., 12, 1367–1380, 2012
https://doi.org/10.5194/nhess-12-1367-2012
Nat. Hazards Earth Syst. Sci., 12, 1367–1380, 2012
https://doi.org/10.5194/nhess-12-1367-2012

Research article 09 May 2012

Research article | 09 May 2012

Recent high-energy marine events in the sediments of Lagoa de Óbidos and Martinhal (Portugal): recognition, age and likely causes

P. J. M. Costa1,2, S. A. G. Leroy2, J. L. Dinis3, A. G. Dawson4, and S. Kortekaas5 P. J. M. Costa et al.
  • 1Centro and Departamento de Geologia, Universidade de Lisboa, Campo Grande, Edifício C6, 1749-016 Lisboa, Portugal
  • 2Institute for the Environment, Brunel University (London), Uxbridge UB8 3PH, UK
  • 3Department of Earth Sciences and IMAR-Marine and Environmental Research Centre, University of Coimbra, Largo Marquês de Pombal, 3000-272 Coimbra, Portugal
  • 4Aberdeen Institute for Coastal Science and Management, University of Aberdeen, Scotland, UK
  • 5Fugro Engineers B.V., Veurse Achterweg 10, P.O. Box 250, 2260 AG Leidschendam, The Netherlands

Abstract. A key issue in coastal hazards research is the need to distinguish sediments deposited by past extreme storms from those of past tsunamis. This study contributes to this aim by investigating patterns of sedimentation associated with extreme coastal flood events, in particular, within the Lagoa de Óbidos (Portugal). The recent stratigraphy of this coastal lagoon was studied using a wide range of techniques including visual description, grain-size analysis, digital and x-ray photography, magnetic susceptibility and geochemical analysis. The sequence was dated by 14C, 210Pb and Optically Stimulated Luminescence. Results disclose a distinctive coarser sedimentary unit, within the top of the sequence studied, and shown in quartz sand by the enrichment of elements with marine affinity (e.g., Ca and Na) and carbonates. The unit fines upwards and inland, thins inland and presents a sharp erosive basal contact. A noticeable post-event change in the sedimentary pattern was observed. The likely agent of sedimentation is discussed here and the conceivable association with the Great Lisbon tsunami of AD 1755 is debated, while a comparison is attempted with a possibly synchronous deposit from a tsunami in Martinhal (Algarve, Portugal). The possibility of a storm origin is also discussed in the context of the storminess of the western Portuguese coast and the North Atlantic Oscillation. This study highlights certain characteristics of the sedimentology of the deposits that may have a value in the recognition of extreme marine inundation signatures elsewhere in the world.

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