Eduardo Méndez Quintas, Manuel Santonja Gómez, Alfredo Pérez González, Martina Demuro, Lee J. Arnold, Mathieu Duval
The geomorphological, geochronological and archaeological investigations developed over the recent years in the lower Miño basin have led to the identification of 9 levels of fluvial terrace and other sedimentary deposits. The sedimentary features indicate stable river patterns over time, which are dominated by a braided gravel model. The earliest human presence in the area has been documented in the intermediate terrace deposits (elevations + 30-39 m and + 21-29 m). They include several archaeological sites characterized by large flake Acheulian lithic assemblages, whose age range between MIS 9 and 6. Finally, additional Middle Palaeolithic sites have also been identified within the terrace deposits +13-17 m, whose inferred age would most likely be between MIS 5 and 4.
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