Las grietas de acantilado como un nuevo registro de tsunamitas : ejemplo en la costa de Gibraltar

Rodríguez Vidal, Joaquín; Cáceres Puro, Luis Miguel; González-Regalado Montero, María Luz; Gómez Gutiérrez, Paula; Ruiz Muñoz, Francisco; Toscano Grande, Antonio; Abad de los Santos, Manuel; Clemente Pérez, María José

Author

Rodríguez Vidal, Joaquín ; Cáceres Puro, Luis Miguel ; González-Regalado Montero, María Luz ; Gómez Gutiérrez, Paula; Ruiz Muñoz, Francisco ; [et al.]
Publication Date

2015
Publisher

Asociación Española para el Estudio del Cuaternario
Citation

Rodríguez Vidal, J., Cáceres Puro, L.M., González-Regalado Montero, M.L., Gómez Gutiérrez, P., Clemente Pérez, M.J., Ruiz Muñoz, F., Toscano Grande, A., Abad de los Santos, M.: "Las grietas de acantilado como un nuevo registro de tsunamitas : ejemplo en la costa de Gibraltar". En: Una visión global del Cuaternario. El hombre como condicionante de procesos geológicos (J. P. Galve, J. M. Azañón, J. V. Pérez Peña y P. Ruano, Eds.), págs. 31-32. XIV Reunión Nacional de Cuaternario, Granada (España).
Abstract

Main tsunami records around the world coasts are associated with low-lying sandy coasts or estuarine areas. In the Rock of Gibraltar formed by limestone cliffs these records are less common and they are limited to the lagoon (The Inundation) located at the isthmus that joins the Rock with the mainland. Tsunamigenic deposits filling deep open crevices that record marine events since ca. 3,000 years BP have been studied at the southwestern end, i.e. Rosia Bay. The most represented deposits could be related with both Atlantic and Mediterranean tsunamis occurred in ~1000 BC, 218-209 BC, 60 AD, 365 AD and 1755 AD. These new tsunamite-type evidence represent a complementary tool in the geological analysis and chronology of these high-energy marine events.
URI

http://hdl.handle.net/10272/11100

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Las grietas de acantilado como un nuevo registro de tsunamitas : ejemplo en la costa de Gibraltar

Author

Rodríguez Vidal, Joaquín UHU Authority

; Cáceres Puro, Luis Miguel UHU Authority

; González-Regalado Montero, María Luz UHU Authority

; Gómez Gutiérrez, Paula; Ruiz Muñoz, Francisco UHU Authority

; [et al.]

Publication Date

2015

Publisher

Asociación Española para el Estudio del Cuaternario

Citation

Rodríguez Vidal, J., Cáceres Puro, L.M., González-Regalado Montero, M.L., Gómez Gutiérrez, P., Clemente Pérez, M.J., Ruiz Muñoz, F., Toscano Grande, A., Abad de los Santos, M.: "Las grietas de acantilado como un nuevo registro de tsunamitas : ejemplo en la costa de Gibraltar". En: Una visión global del Cuaternario. El hombre como condicionante de procesos geológicos (J. P. Galve, J. M. Azañón, J. V. Pérez Peña y P. Ruano, Eds.), págs. 31-32. XIV Reunión Nacional de Cuaternario, Granada (España).

Abstract

Main tsunami records around the world coasts are associated with low-lying sandy coasts or estuarine areas. In the Rock of Gibraltar formed by limestone cliffs these records are less common and they are limited to the lagoon (The Inundation) located at the isthmus that joins the Rock with the mainland. Tsunamigenic deposits filling deep open crevices that record marine events since ca. 3,000 years BP have been studied at the southwestern end, i.e. Rosia Bay. The most represented deposits could be related with both Atlantic and Mediterranean tsunamis occurred in ~1000 BC, 218-209 BC, 60 AD, 365 AD and 1755 AD. These new tsunamite-type evidence represent a complementary tool in the geological analysis and chronology of these high-energy marine events.

URI

http://hdl.handle.net/10272/11100

Fichero	Tamaño	Formato	Ver	Description
Las_grietas_de_acantilado.pdf	420.6Kb	PDF	View/Open	There is no description for this item

Fichero	Tamaño	Formato	Ver	Description
Las_grietas_de_acantilado.pdf	420.6Kb	PDF	View/Open	There is no description for this item