Paleotsunami Evidence in the Bahía Inglesa Coast (Atacama, Chile) Based on a Multi-Approach Analysis

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Paleotsunami Evidence in the Bahía Inglesa Coast (Atacama, Chile) Based on a Multi-Approach AnalysisAuthor(s)
Date
2022-02-24Citation
Carballeira, R., Peña-Monne, J.L., Otero, X.L. et al. Paleotsunami evidence in the Bahía Inglesa coast (Atacama, Chile) based on a multi-approach analysis. Environ Earth Sci 81, 153 (2022). https://doi.org/10.1007/s12665-022-10259-2
Abstract
[Abstract] The Atacama coast is located in an area with a current high risk of tsunami, and the sedimentary deposits found in the Bahía Inglesa area, in the Morro sector, clearly indicate that this was also the case in the past. This investigation analyzes a paleotsunami sedimentary deposit consisting of a block field associated with three sand lobes oriented towards land on top of a marine terrace at an altitude of 70–75 m, which originated from a tsunamigenic event occurred between interglacial periods MIS 7 (ca. 210 ± 10 ky) and MIS5e (ca. 125 ± 5 ky). The deposits have been studied using a multiple approach combining geomorphological, sedimentological, biological, and geochemical criteria. The first type of criteria clearly indicate that the energy required to move the blocks and form the sand lobes could only have been generated by a tsunami. Sedimentological criteria constitute direct evidences of a marine origin due to the presence of siliceous remains from diatom species and spicules from strictly marine sponges, while geochemical criteria, such as the stable isotope signature and chemical composition, constitute evidence of a marine intrusion.
Keywords
Atacama desert coast
Tsunami
Cliff-top boulder deposit
Marine terraces
Geomorphology
Geochemical signature
Diatoms
Tsunami
Cliff-top boulder deposit
Marine terraces
Geomorphology
Geochemical signature
Diatoms
Description
Financiado para publicación en acceso aberto: Universidade da Coruña/CISUG
Editor version
Rights
Atribución 4.0 Internacional
ISSN
1866-6299
1866-6280
1866-6280