A terrace formation model (TERRACE) combined with a longitudinal river profile model
(FLUVER) was used to simulate fluvial terrace formation and preservation in the northwest …

The origin of the lower Miño River terraces in the NW Iberian Peninsula has been a topic of
debate since the 1940s. Various hypotheses about their main controlling factors have been …

Many river systems in western North America retain a fluvial strath-terrace rec ord of
discontinuous downcutting into bedrock through the Quaternary. Their importance lies in …

Geostatistical topographic analysis is widely recognized as a useful tool for the statistical
reconstruction of planar geomorphic markers from relict surfaces. This work is aimed at …

Terraces eroded into sediment (alluvial) and bedrock (strath) preserve an important history
of river activity. River terraces are thought to form when a river switches from a period of slow …

The southern foreland basin of the Pyrenees (Ebro basin) is an exorheic drainage basin
since Late Miocene times. Remnants of an early exorheic Ebro drainage system are not …

The study of drainage network response to uplift is important not only for understanding river
system dynamics and associated channel properties and fluvial landforms, but also for …

At the geological time scale, the way in which the erosion of drainage catchments responds
to tectonic uplift and climate changes depends on boundary conditions. In particular …

We present a forward-modelling case study for the development of the longitudinal profile of
a basin–marginal fluvial system (River Meuse, NW Europe) responding to Late Quaternary …

How rock resistance or erodibility affects fluvial landforms and processes is an outstanding
question in geomorphology that has recently garnered attention owing to the recognition that …