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 …

We have used fluvial (Solent River system) and marine terraces to reconstruct the uplift
history of central southern England. In the case of the former, we make the assumption that …

Active fault traces are a surface expression of permanent deformation that accommodates
the motion within and between adjacent tectonic plates. We present an updated national …

The timing of the development of strath terraces with respect to climatic variability remains
equivocal. Previous studies attribute strath-terrace formation to glacial or interglacial …

It is widely recognised that the acquisition of high‐resolution palaeoclimate records from
southern mid‐latitude sites is essential for establishing a coherent picture of inter …

Published by the American Geophysical Union as part of the Water Resources Monograph
Series, Volume 19. What are the forms and processes characteristic of mountain rivers and …

The Southern Hemisphere westerlies in the southwest Pacific are known to have waxed and
waned numerous times during the last two glacial cycles, though even semi-continuous …

Deformed fluvial terraces preserved over active thrust‐related folds record the kinematics of
folding as fault slip accumulates on the underlying thrust. In the Mackenzie Basin of southern …

Field observations from western Washington and eastern Tibet indicate a strong lithologic
influence on strath terrace formation and highlight the response of bedrock channel width to …

The uplift rate and pattern of the Qilian Shan Mountain, which lies in the northeast margin of
the Tibetan Plateau, are key to understanding the dynamics of crustal deformation in the …