We analyzed the sedimentary record of the westerm sector of the Seville historical town, from a geoarcheological point of view. We study the sequence of the centuries. Furthemore, the stages of the historical palaeogeographic evolution of the urban sector affected by change of place of these meander settle down, identifying three main episodes: a phase of fast meander movement (Roman time); a phase of alluvial reactivation of the floodplain (Roman-Medieval transition); and a phase of hidro-dynamic stability with edaphic traces (Final medieval epoch).
Key words: point bar deposits, Guadalquivir floodplain, Geoarchaeology.