Quaternary uplift of many coastal regions is revealed by sequences of marine terraces. In
many localities this uplift relates to tectonic deformation caused by plate motions. However …

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 …

Rivers are continuously present in areas with humid climatic conditions. Their evolution is
recorded in sediment-landform assemblages. Over the years, several river-terrace flights …

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 …

Geomorphic processes that produce and transport sediment, and incise river valleys are
complex; and often difficult to quantify over longer timescales of 10 3 to 10 5 y. Morphometric …

Long-term river terrace sequences reveal that many regions have uplifted by several
hundred metres since the Middle Pliocene. They indeed provide evidence of a global …

It is still debated whether the primary control on the middle Pleistocene denudation of the
uplifted Ardennes massif (western Europe) is tectonic or climatic. Here, based on …

The Meuse river system is located in the northeastern part of the Paris Basin, the Ardennes,
and the Roer Valley Rift System (RVRS). The Meuse river system developed during the uplift …

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 …

The north Alpine foreland basin extends from French Savoy in the west to the Linz area of
Austria in the east and parallels the Alpine front. In eastern Switzerland, Bavaria and Austria …