“…Typical Mousterian without Acheulean or Upper Palaeolithic influence, that is, Levallois and discoidal technology with centripetal and knapped pebbles, Levallois and pseudo-Levallois blanks, notches, denticulates and sidescrapers, occurs at many terrace sites of the Lower River Tejo with ages similar to or younger than the base of T5 (135 ka) and the sequence of T6 (younger than 32 ka). These include Caminho da Celulose (Cunha et al, 2008;G.E.P.P., 1977), Vilas Ruivas (Cunha et al, 2008;Raposo, 1995), Ribeira da Atalaia -T5 top (Cura, 2014;Rosa, 2013;Rosina et al, 2014), Estrada do Prado (Mateus, 1984), Santa Cita (Bicho and Ferring Reid, 2001;Lussu et al, 2001), Conceição (Raposo and Cardoso, 1998) and Santo Antão do Tojal (Cunha et al, 2017b;Raposo, 1995), Campo de Futebol de Santo Antão do Tojal (Figueiredo et al, 2005), Azinhal and Tapada do Montinho (Almeida, 2014(Almeida, , 2013Almeida et al, 2007;Cunha et al, 2017bCunha et al, , 2017aCunha et al, , 2016, and Foz do Enxarrique (Berruti et al, 2016;Cardoso, 1993;Cunha et al, 2008;Martins et al, 2010a;Raposo, 1995;Raposo et al, 1985;Raposo and Brugal, 1999).…”