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IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy<br />

(S) - <strong>IASPEI</strong> - International Association of Seismology and Physics of the Earth's<br />

Interior<br />

JSS002 Oral Presentation 1734<br />

Geological recognition of tsunami and storm deposits in two coastal areas<br />

of Portugal<br />

Mr. Pedro J M Costa<br />

Earthquake Engineering and Seismology Division, IC IST Technical University of Lisbon<br />

Suzanne A. G. Leroy<br />

Abrupt marine invasions such as tsunamis and storms are particularly devastating for coastal areas.<br />

They may also leave a permanent record in sedimentary deposits. In historical times the most<br />

destructive tsunami that affected Europe was the Lisbon AD 1755. The effects and consequences of the<br />

AD 1755 tsunami are presented. Sedimentological criteria to identify abrupt marine invasions in the<br />

stratigraphic column are discussed. This work aims to contribute to a better understanding of the<br />

signature left by abrupt marine invasions in coastal stratigraphy by investigating the nature of the<br />

sedimentary record associated with tsunamis in a region of their known impact. A wide range of proxies<br />

was used to detected tsunami and storm deposits in two coastal areas of Portugal. The techniques used<br />

include stratigraphic description, grain size analysis, digital and x-ray photography, magnetic<br />

susceptibility, macrofossils analysis, geochemical analysis and 210Pb and Optically Stimulated<br />

Luminescence dating. The investigated areas (e.g. Lagoa de bidos (Central Portugal) and Martinhal<br />

(South Portugal)) were affected by the AD 1755 tsunami. The locations have similar geomorphological<br />

features and are both susceptible to major abrupt marine invasions. Results show that an abrupt event<br />

deposited unique sedimentary units in both locations. A similar age for the event was established. A<br />

considerable number of tsunami sedimentary characteristics were detected in both units. Moreover,<br />

other abrupt marine invasions were detected in the lithostratigraphy of the study areas. However, a key<br />

outcome of this research is the demonstration of the difficulty of distinguishing between sedimentary<br />

deposits laid down by tsunamis, and those deposits resulting from storm action; consequently the<br />

geological record of tsunamis almost certainly underestimates their frequency.<br />

Keywords: tsunami, storms, portugal

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