Late Cenozoic environmental changes which affected European rivers are reviewed,
focusing especially on those of mid-Pleistocene times (c. 1.2–0.8 Ma or around MIS 22) and …

Staircases of large-scale aggradational river terraces are a notable feature of many valleys
in the temperate lattitudes, particularly in areas beyond the reach of the erosive activities of …

Based on the interpretation of geophysical data (very high resolution seismic data combined
with EM1000 swath bathymetry), this paper reviews the history of the Channel River …

In glaciated continental basins accommodation space is not only controlled by tectonics and
sea-level but also by the position of ice-sheets, which may act as a regional base-level for …

This paper reviews the occurrence, structure, stratigraphy and development of the principal
deposits of the Rivers Dniester, Dnieper, Don and Volga. Such archives occur as alluvial …

The Medway is a river of considerable antiquity that has had an important role within the
evolution of drainage in southeast England. Its upper catchment has expanded during the …

The Pleistocene history of river systems that enter the English Channel from northern France
and southern England is reviewed. During periods of low sea‐level (cold stages) these …

Effects of flow in the lower continental crust have often been ignored in the
geomorphological literature on the growth of topography during the Quaternary. However …

Detailed fieldwork and new extensive 14C dating of residual channel infillings provide data
for the reconstruction of the Late‐glacial channel downcutting and incision history of the …

Much of the past work on the Quaternary rivers of northwest Europe has been concerned
with river terraces, which characterise almost every valley. While these terraces are …