Rivers are extremely sensitive to subtle changes in their grade caused by tectonic tilting. As
such, recognition of tectonic tilting effects on rivers, and their resultant sediments, can be a …

The major goal of this book is to bring together evidence of active deformation on alluvial
rivers, with emphasis on geomorphological adjustment. The authors have grouped their …

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 …

Along three rivers at the Mendocino triple junction, northern California, strath, cut, and fill
terraces have formed in response to tectonic and eustatic processes. Detailed surveying and …

Alluvial rivers respond to valley-slope deformation caused by active tectonics in various
ways depending on the rate and amount of surficial deformation and on the type of river. On …

Many active compressional belts contain examples of transverse rivers intersecting
anticlines at their highest structural and topographic position. This unusual association …

Alluvial rivers are influenced by changes of valley floor slope, and therefore deformation of
the valley floor by active tectonics can cause pattern change, aggradation, and degradation …

The mode of channel‐bend transformation (ie expansion, translation, rotation or a
combination thereof) has a direct bearing on the dimensions, shape, bedding architecture …

First-generation sequence stratigraphic models have dealt in a very rudimentary fashion
with the response of fluvial systems to eustasy. A major element of presently accepted …

We present detailed data of channel morphology for a river undergoing a transient response
to active normal faulting where excellent constraints exist on spatial and temporal variations …