Abstract

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.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.