Boulder deposition during major tsunami events

Cesar Andrade, Maria C Freitas, Maria A. Oliveira, Carlos M. da Silva, Rachid Omira, Rui Taborda, Maria A. Baptista, Pedro J.M. Costa

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24 Citations (Scopus)

Abstract

Remarkable accumulations of marine boulders located above present spring tide level occur in two coastal lowlands of the Algarve (Portugal). The size-interval of particles studied here is seldom reported in the literature in association with extreme events of coastal inundation, thus making this study of relevance to many other coasts worldwide.The spreads of boulders extend several hundred meters inland and well beyond the present landward limit of storm activity. The marine origin of the boulders is demonstrated by well-developed macro-bioerosion sculpturing and in situ skeletal remains of endolithic shallow marine bivalves. The good state preservation of the fossils within the boulders indicates that abrasion during transport and redeposition was not significant. We envisage boulder deposition as having taken place during the Lisbon tsunami of AD 1755 through the simultaneous landward entrainment of coarse particles from nearshore followed by rapid shoreward suspended-dominated transport and non-graded redeposition that excluded significant sorting by weight or boulder dimensions. We use numerical hydrodynamic modeling of tsunami (and storm) waves to test the observational data on boulder dimensions (density, size, distribution) on the most likely processes of sediment deposition.
Original languageEnglish
Pages (from-to)2054-2068
Number of pages15
JournalEarth Surface Processes and Landforms
Volume36
Issue number15
Early online date28 Sep 2011
DOIs
Publication statusPublished - Dec 2011

Keywords

  • boulders
  • storm
  • tsunami
  • sediment transport
  • bioerosion
  • AD 1755
  • Portugal

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    Andrade, C., Freitas, M. C., Oliveira, M. A., da Silva, C. M., Omira, R., Taborda, R., Baptista, M. A., & Pedro J.M. Costa (2011). Boulder deposition during major tsunami events. Earth Surface Processes and Landforms, 36(15), 2054-2068. https://doi.org/10.1002/esp.2228