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Post last glacial maximum (LGM) shoreline evolution in the Algarve (south Portugal)
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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.
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Moura, D.; Albardeiro, L.; Veiga-Pires, C.; Boski, T.Post last glacial maximum (LGM) shoreline evolution in the Algarve (south Portugal), Trabalho apresentado em Joint INQUA-IGCP 495 Meeting, In Abstract Book: A joint INQUA-IGCP 495 Meeting, Dunkerque, France, 2005.