Statistical analysis of the morphology of pebbles in Pleistocene alluvial deposits of the Adour-Arros river region, between Vic-en-Bigorre and Aire-sur-l'Adour, France, permitted formulation of a set of parameters on the basis of which distance of transport and relationships between the different Riss and Wuerm (Pleistocene) sheets are interpreted. The Adour captured the Arros at the end of the Riss.

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