Abstract Analysis of three-dimensional morphological properties of 24 coastal drainage
basins that have evolved in areas of low (< 1 m/1,000 yr), intermediate (1-3 m/1,000 yr), and …

A landscape records the surface response to tectonics at time scales intermediate between
short time-scale information derived from seismic imaging and global positioning systems …

Abstract Analysis of the altitudinal spacing of 14 flights of marine terraces indicates a spatial
pattern of varying uplift rates that agrees with that determined from previously dated terraces …

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 …

Channel migration and meander-bend morphology are examined for the lower Mississippi
River between 1877 and 1924, prior to channel cutoffs, revetments, and change in sediment …

An empirical calibration of the shear stress model for bedrock incision is presented, using
field and hydrologic data from a series of small, coastal drainage basins near the Mendocino …

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 …

Lateral migration fluvial meander belts preserves wider than normal coarse-sediment
bodies, asymmetric meander belts, that have a complex architecture recording the history of …

The topographic evolution of orogens is fundamentally dictated by rates and patterns of
bedrock-channel incision. Quantitative field assessments of process-based laws are needed …

An examination of the response of the Lower Mississippi River (LMR) to a variety of
engineering activities is presented through the discussion of:(a) a brief history of …