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An amalgamated meter-thick sedimentary package enabled by the 2011 Tohoku tsunami in El Garrapatero, Galapagos Islands

Published online by Cambridge University Press:  20 January 2017

Maria Elizabeth Martin Arcos ,
BreanynTiel MacInnes ,
Patricia Arreaga ,
Frances Rivera-Hernandez ,
Robert Weiss  and
Patrick Lynett
Maria Elizabeth Martin Arcos*
Affiliation:
AMEC, 2101 Webster Street, Oakland, CA 94612, USA
BreanynTiel MacInnes
Affiliation:
Dept. of Geological Sciences, Central Washington University, 400 E. University Way (7418), Ellensburg, WA 98926, USA
Patricia Arreaga
Affiliation:
InstitutoOceanogr"fico de la Armada de Ecuador, Av. 25 de Julio-km 3 1/2 v"aPto. Mar"timo Base Naval Sur, Guayaquil, Ecuador
Frances Rivera-Hernandez
Affiliation:
Department of Earth and Space Sciences, University of Washington, Box 351310, Seattle, WA 98195-1310, USA
Robert Weiss
Affiliation:
Department of Geosciences, Virginia Tech, 4044 Derring Hall (0420), Blacksburg, VA 24061, USA,
Patrick Lynett
Affiliation:
Department of Civil and Environmental Engineering, University of Southern California, Los Angeles, CA 90089-2531, USA
*
*Corresponding author. Fax: + 1 510 663 4141. E-mail address:[email protected] (M.E.M. Arcos).
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Abstract

Tsunamis and storms instigate sedimentological and geomorphological changes to the coastal system, both long-term and ephemeral. To accurately predict future coastal hazards, one must identify the records that are generated by the processes associated with these hazards and recognize what will be preserved. Using eyewitness accounts, photographs, and sedimentology, this study documents pre- and post-tsunami conditions and constrains the timing and process of depositional events during and following the 11 March 2011 Tohoku tsunami in the coastal system at El Garrapatero, Galapagos Islands. While the tsunami acted as both an erosional and depositional agent, the thick, fan-like sand sheet in El Garrapatero was primarily emplaced by overwash deposition during high tide from swell waves occurring between 19–25 March and 17–22 April 2011. The swell waves were only able to access the terrestrial coastal system via a channel carved by the 2011 Tohoku tsunami through the barrier sand dune. This combined deposit could result in an overestimation of the hazard if interpreted to be the result of only one event (either tsunami or wind-generated waves). An analogous sand layer, younger than 1390–1530 calyr BP, may record a similar, prior event.

Keywords

Tsunami depositsCoastal morphologyNatural hazards
Type
Original Articles
Information
Quaternary Research , Volume 80 , Issue 1 , July 2013 , pp. 9 - 19
Copyright
University of Washington

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