Presence of boulders associated with an extreme wave event in the western Mediterranean, Cape Cope, Murcia, Spainpossible evidence of a tsunami
- Javier Lario 1
- Chris Spencer 2
- Teresa Bardají 3
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1
Universidad Nacional de Educación a Distancia
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- 2 UWE Bristol
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3
Universidad de Alcalá
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ISSN: 1886-7995, 1698-6180
Año de publicación: 2023
Volumen: 49
Número: 2
Páginas: 115-132
Tipo: Artículo
Otras publicaciones en: Journal of iberian geology: an international publication of earth sciences
Resumen
La región de Murcia, en el sureste de la Península Ibérica, registra una actividad tectónica moderada, registrándose terremotos de hasta 6,2-6,9 Mw. Aún con una actividad sísmica de esta magnitud no existen registros geológicos ni instrumentales de tsunamis que hayan afectado a la zona. La presencia en Cabo Cope, Murcia, de un cordón litoral de bloques imbricados de tamaño métrico (compuestos por rocas del Pleistoceno superior) que alcanzan una altura de hasta 4 m sobre el nivel del mar, indica que en la zona se ha producido un evento de oleaje extremo durante el Holoceno. Mediante el estudio de las condiciones de oleaje generadas durante grandes tormentas en esta zona, se infere que este cordón litoral de bloques parece haber sido causado por oleaje extremo asociado a un evento sísmico, como un tsunami.
Información de financiación
Financiadores
- University of the West of England
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Ministerio de Ciencia, Innovación y Universidades
- CGL2015-69919-R
- Universidad Nacional de Educacion Distancia
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