THE GEOLOGICAL RECORD OF THE OLDEST HISTORICAL TSUNAMIS IN SOUTHWESTERN SPAIN
A regressive sequence was determined in the late Holocene evolution of the southwestern Doñana National Park (SW Spain), based on a multidisciplinary study of sediments obtained in a drill core. In an initial phase (> cal. 2400 years BP), a shallow coastal lagoon with a partial marine connection...
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Università degli Studi di Milano
2008-03-01
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doaj-9213fd8d920f4470abc0a69108bf12eb2020-11-24T23:28:06ZengUniversità degli Studi di MilanoRivista Italiana di Paleontologia e Stratigrafia0035-68832039-49422008-03-01114110.13130/2039-4942/63735684THE GEOLOGICAL RECORD OF THE OLDEST HISTORICAL TSUNAMIS IN SOUTHWESTERN SPAINFRANCISCO RUIZMANUEL ABADJOAQUÍN RODRÍGUEZ VIDALLUIS MIGUEL CÁCERESMARÍA LUZ GONZÁLEZ-REGALADOMARÍA ISABEL CARRETEROMANUEL POZOFRANCISCO GÓMEZ TOSCANOA regressive sequence was determined in the late Holocene evolution of the southwestern Doñana National Park (SW Spain), based on a multidisciplinary study of sediments obtained in a drill core. In an initial phase (> cal. 2400 years BP), a shallow coastal lagoon with a partial marine connection occupied this area, with a progressive transition from subtidal to supratidal conditions. The following phase (cal. 2400-2350 years BP) is characterized by a tsunami, with the deposition of an upper chenier. This sedimentological layer is characterized by a ridge morphology, an erosive base, high bioclastic contents and the introduction of marine species toward the inner areas of this old lagoon. This tsunami may be assimilated to one of the historical tsunamis that occurred between 218 and 209 BC. A comparison with other deposits derived from these high-energy events permits to draw the differential effects produced along the western Iberian coasts. SHORT NOTEShttps://riviste.unimi.it/index.php/RIPS/article/view/6373Estuarine evolutionTsunami depositsLate HoloceneSW SpainPortugal |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
FRANCISCO RUIZ MANUEL ABAD JOAQUÍN RODRÍGUEZ VIDAL LUIS MIGUEL CÁCERES MARÍA LUZ GONZÁLEZ-REGALADO MARÍA ISABEL CARRETERO MANUEL POZO FRANCISCO GÓMEZ TOSCANO |
spellingShingle |
FRANCISCO RUIZ MANUEL ABAD JOAQUÍN RODRÍGUEZ VIDAL LUIS MIGUEL CÁCERES MARÍA LUZ GONZÁLEZ-REGALADO MARÍA ISABEL CARRETERO MANUEL POZO FRANCISCO GÓMEZ TOSCANO THE GEOLOGICAL RECORD OF THE OLDEST HISTORICAL TSUNAMIS IN SOUTHWESTERN SPAIN Rivista Italiana di Paleontologia e Stratigrafia Estuarine evolution Tsunami deposits Late Holocene SW Spain Portugal |
author_facet |
FRANCISCO RUIZ MANUEL ABAD JOAQUÍN RODRÍGUEZ VIDAL LUIS MIGUEL CÁCERES MARÍA LUZ GONZÁLEZ-REGALADO MARÍA ISABEL CARRETERO MANUEL POZO FRANCISCO GÓMEZ TOSCANO |
author_sort |
FRANCISCO RUIZ |
title |
THE GEOLOGICAL RECORD OF THE OLDEST HISTORICAL TSUNAMIS IN SOUTHWESTERN SPAIN |
title_short |
THE GEOLOGICAL RECORD OF THE OLDEST HISTORICAL TSUNAMIS IN SOUTHWESTERN SPAIN |
title_full |
THE GEOLOGICAL RECORD OF THE OLDEST HISTORICAL TSUNAMIS IN SOUTHWESTERN SPAIN |
title_fullStr |
THE GEOLOGICAL RECORD OF THE OLDEST HISTORICAL TSUNAMIS IN SOUTHWESTERN SPAIN |
title_full_unstemmed |
THE GEOLOGICAL RECORD OF THE OLDEST HISTORICAL TSUNAMIS IN SOUTHWESTERN SPAIN |
title_sort |
geological record of the oldest historical tsunamis in southwestern spain |
publisher |
Università degli Studi di Milano |
series |
Rivista Italiana di Paleontologia e Stratigrafia |
issn |
0035-6883 2039-4942 |
publishDate |
2008-03-01 |
description |
A regressive sequence was determined in the late Holocene evolution of the southwestern Doñana National Park (SW Spain), based on a multidisciplinary study of sediments obtained in a drill core. In an initial phase (> cal. 2400 years BP), a shallow coastal lagoon with a partial marine connection occupied this area, with a progressive transition from subtidal to supratidal conditions. The following phase (cal. 2400-2350 years BP) is characterized by a tsunami, with the deposition of an upper chenier. This sedimentological layer is characterized by a ridge morphology, an erosive base, high bioclastic contents and the introduction of marine species toward the inner areas of this old lagoon. This tsunami may be assimilated to one of the historical tsunamis that occurred between 218 and 209 BC. A comparison with other deposits derived from these high-energy events permits to draw the differential effects produced along the western Iberian coasts.
SHORT NOTES |
topic |
Estuarine evolution Tsunami deposits Late Holocene SW Spain Portugal |
url |
https://riviste.unimi.it/index.php/RIPS/article/view/6373 |
work_keys_str_mv |
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