The low terrace of the Seine in the meander of Elbeuf presents three periglacial alluvial deposits and interglacial estuarine formations intercalated, the whole sequence being dated from Saalian. The fauna of great mammals is well represented: among
Reconstitution de l'évolution géomorphologique dominée par la tectonique qui a modifié les niveaux de base et par les changements climatiques. Le jeu de la tectonique a permis l'incision très profonde des vallées suivie d'un remplissage alluvial. Le
La très basse nappe alluviale de la Seine dans la région du site archéologique de Pincevent (Montereau, Seine-et-Marne). in Colloque AFEQ, Paris 1983. (The lower alluvial layer of the river Seine in the region of the archeological site of Pincevent
Un manteau alluvial holocène d'une trentaine de mètres d'épaisseur témoigne que le bassin amazonien était soumis à de fortes inondations saisonnières entre 11000 et 5000 BP environ, période qui fut suivie par deux cycles d'érosion-accumulation. Si
An occurate analysis of the würmian fluvioglacial drift of the river Durance shows the combination of alluviations during the glacial progression and during the first part of the glacial recession. However, as well as in the Rhône valley near Lyon
The two graded megasequences observed in the alluvial deposits (middle terrace) of the river Moselle, with the help of other sedimentological indicators, allow the author to correlate sedimentation periods and climatic cycle: sedimentation occurs
Sedimentary and erosional phases responsible for the formation of fluviatile terraces are studied in a middle altitude environment. The importance of neotectonic phenomena is revealed by the shaping of alluvial channels as also their sedimentary
After the deposit of Würmian alluvium (lower terrace of 15-20 m), one can distinguish two phases of in cutting during the Late Glacial followed by a period of alluviation which stops during the Atlantic. Then, the Allier river hollows her present