“…In more distal areas of the piedmont, particularly downstream of Toulouse in the case of the Garonne River, the treads of T1 and T0 become topographically indistinct. Stratigraphic analysis of this low plain has revealed a complex Lateglacial and Holocene history involving a succession of many aggradational and incisional phases (Bruxelles et al, 2010;Carrozza et al, 2013).…”