Autor(es):
Moura, Delminda 
; Albardeiro, L. ; Veiga-Pires, C. ; Boski, T.
Data: 2005
Identificador Persistente: http://hdl.handle.net/10400.1/2778
Origem: Sapientia - Universidade do Algarve
Detalhes do Documento
Post last glacial maximum (LGM) shoreline evolution in the Algarve (south Portu...
Descrição
Aeolianites spanning the last 20 ka, are outcropping in a different geomorphological context along the Algarve coast, South Portugal. Here we use the term aeolianite as defined by Fairbidge and Johnson (1978), being a wind-blown sediment originating from the beach with a high carbonate content. The therefore it is related with sea-level fluctuations. However, other factors like coastal plain slope, marine environment, and coastal morphology, influence the morphogenetic processes.
Aeolianites spanning the last 20 ka, are outcropping in a different geomorphological context along the Algarve coast, South Portugal. Here we use the term aeolianite as defined by Fairbidge and Johnson (1978), being a wind-blown sediment originating from the beach with a high carbonate content. The therefore it is related with sea-level fluctuations. However, other factors like coastal plain slope, marine environment, and coastal morphology, influence the morphogenetic processes.
Tipo de Documento
Documento de conferência
Idioma Inglês
Idioma Inglês
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