The competing roles of bedrock uplift and climatic change in the formation of fluvial terraces
remain uncertain. Most of recent studies have attributed terrace formation to climatic …

Sediment deposition in floodplains is an essential part of the sediment dynamics of a
catchment. These sediment dynamics can vary largely on a Holocene time scale under the …

Rivers self-organize their pattern/planform through feedbacks between bars, channels,
floodplain and vegetation, which emerge as a result of the basic spatial sorting process of …

Abstract Late Cenozoic (and especially Quaternary) fluvial deposits and related landforms
provide valuable information about landscape evolution, not just in terms of changing …

This paper discusses the potential response of fluvial processes and landforms to the
projected permafrost degradation and related hydrological change. Fluvial system structure …

Climate impact on the fluvial processes led to morphological and sedimentological
differentiation of a terrace. This diversity in the fluvial environment determined how people …

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 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 …

Thirty-three lowland floodplains and their associated delta plains are characterized with data
from three remote sensing systems (AMSR-E, SRTM and MODIS). These data provide new …

Cohesive floodplain sediment and vegetation are both thought to cause meandering river
patterns. Our aims are to compare the isolated and combined effects of mud and vegetation …