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This paper shows the stratigrafhic alluvial and post-alluvial sequence of the "Muharra terrace" included into the High Terrace Complex of Guadalquivir river. Its origin is linked to two different episodies: one related to the sedimentation of the River; a second one, post-aluvial, with the development of hydromorphic processes and a insert paleo-soil. The research of the abundant lithic industry collected in that secuence (more than 450 pieces), allowed us to clasify it, as a deposit of Transitional Achalense, placed in a confined environment (level 4). The secuence shows signs that might correspond to "achalense" in general terms, in the lower levels (included the aluvial ones).

Secuencia aluvial y post-aluvial de la terraza de Muharra (Carmona, Sevilla): Aportación al Achelense en el valle del Guadalquivir