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Discussion papers | Copyright
https://doi.org/10.5194/nhess-2018-62
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 12 Mar 2018

Research article | 12 Mar 2018

Review status
This discussion paper is a preprint. A revision of the manuscript was accepted for the journal Natural Hazards and Earth System Sciences (NHESS).

Paleotsunami deposits along the coast of Egypt correlate with historical earthquake records of eastern Mediterranean

Asem Salama1,2,a, Mustapha Meghraoui1, Mohamed El Gabry2,a, Said Maouche3,a, Hesham Moussa Hussein2,a, and Ibrahim Korrat4 Asem Salama et al.
  • 1EOST-IPGS – CNRS – UMR 7516, 5 rue René Descartes, Strasbourg, France
  • 2NRIAG, 11421 Helwan, Egypt
  • 3CRAAG, Bouzareah, Algeria
  • 4Dept. of Seismology, Mansoura University, Mansoura, Egypt
  • aalso at: North Africa Group for Earthquake and Tsunami Studies (NAGET), Ne t40/OEA ICTP, Italy

Abstract. We study the sedimentary record of past tsunamis along the coastal area west of Alexandria (NW Egypt) taking into account the occurrence of major historical earthquakes in the eastern Mediterranean. The two selected sites at Kefr Saber (~32-km west of Marsa-Matrouh city) and ~10km northwest of El Alamein village are coastal lagoons protected by 2 to 20-m-high dunes parallel to the shoreline. Field data were collected by: (1) Coastal geomorphology along estuaries, wedge-protected and dune-protected lagoons, and (2) identification of paleotsunamis deposits and their spatial distribution using five trenches (1.5-m-depth) at Kefr Saber and twelve cores (1 to 2.5-m-depth) at El Alamein. Detailed logging of sedimentary sections were analysed using X rays, grain size and sorting, total organic and inorganic matter, bulk mineralogy, magnetic susceptibility and radiocarbon dating necessary for the identification of past tsunamis records. Generally of low energy, the stratigraphic succession made of marine and alluvial deposits includes intercalated high-energy deposits made of mixed fine and coarse sand with broken shells, interpreted as catastrophic layers correlated with tsunami deposits. Although the radiocarbon dating of 46 samples consist in mixed old (>13000yearBP) and young (<5500yearBP), dated charcoal and shell in sedimentary units allow the correlation with the 24 June 1870 (Mw7.5), 8 August 1303 (Mw~8) and 21 July 365 (Mw8–8.5) large tsunamigenic earthquakes that caused inundations in Alexandria and northern Egyptian shoreline. Our results point out the size and recurrence of past tsunamis and the potential for tsunami hazard over the Egyptian coastline and the eastern Mediterranean regions.

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We study the sedimentary record of past tsunamis along the coastal area west of Alexandria (NW Egypt) taking into account the occurrence of major historical earthquakes in the eastern Mediterranean. Dated charcoal and shell in sedimentary units allow the correlation with the 1870 (Mw 7.5), 1303 (Mw ~ 8) and 365 (Mw ~ 8) large tsunamigenic earthquakes. Our results point out the size and recurrence of past tsunamis and the potential for tsunami hazard over the Egyptian coastline.
We study the sedimentary record of past tsunamis along the coastal area west of Alexandria (NW...
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