Geomorphological constraining of tsunami (?) run-up in the Alcantarilha coastal lowland (Central Algarve, Portugal)

The Alcantarilha lowland, partly barred by a well developed barrier, including foredunes covering Pleistocene-Holocene beachrock and aeolianite, develops across the Alcantarilha infilled estuary, the beach-dune extending further SE until the Salgados lagoon. A topographic and coring survey revealed...

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Detalhes bibliográficos
Autor principal: Dinis, Jorge (author)
Outros Autores: Andrade, César (author), Oliveira, Alexandre (author), Freitas, Maria (author), Cunha, Pedro (author), Martins, António (author), Costa, Pedro (author)
Formato: article
Idioma:por
Publicado em: 2016
Assuntos:
Tsunami run up
Alcantarilha coastal
Algarve
trenches
Texto completo:http://hdl.handle.net/10174/18476
País:Portugal
Oai:oai:dspace.uevora.pt:10174/18476

Texto Completo

http://hdl.handle.net/10174/18476

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