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Presence of boulders associated with an extreme wave event in the western Mediterranean (Cape Cope, Murcia, Spain): Possible evidence of a tsunami

Lario, Javier; Spencer, Chris; Bardají, Teresa

Presence of boulders associated with an extreme wave event in the western Mediterranean (Cape Cope, Murcia, Spain): Possible evidence of a tsunami Thumbnail


Authors

Javier Lario

Teresa Bardají



Abstract

The region of Murcia, in the southeast of the Iberian Peninsula, experiences moderate tectonic activity, with earthquakes of up to 6.2–6.9 Mw recorded. Even with seismic activity of this scale there is no geological or instrumental record of tsunamis affecting the area. The presence at Cape Cope, Murcia of a ridge of metre-sized imbricated boulders (comprised of Upper Pleistocene sediments) reaching a height of up to 4m above sea level, indicates that there has been an extreme wave event in the area during the Holocene. Through studying the wave conditions generated during large storms in this area, the boulder ridges appear to have been caused by extreme waves associated with a seismic event, as a tsunami.

Journal Article Type Article
Acceptance Date Mar 1, 2023
Online Publication Date Mar 20, 2023
Publication Date Jun 1, 2023
Deposit Date Jun 6, 2023
Publicly Available Date Jun 7, 2023
Journal Journal of Iberian Geology
Print ISSN 1698-6180
Electronic ISSN 1886-7995
Publisher Springer
Peer Reviewed Peer Reviewed
Volume 49
Issue 2
Pages 115-132
DOI https://doi.org/10.1007/s41513-023-00208-8
Keywords Extreme wave event, Registro geológico, Transporte de bloques, Evento de oleaje extremo, Boulders transport, Tsunami, Geological record
Public URL https://uwe-repository.worktribe.com/output/10835781
Publisher URL https://link.springer.com/article/10.1007/s41513-023-00208-8

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