There is a coincidence of seismicity and major river valleys in the southwestern Mississippi
Embayment that suggests control of the drainage pattern by northwest-trending faults …

To investigate neotectonism in the Mississippi Embayment east of the New Madrid seismic
zone, we identified geomorphic domains that show evidence of ground tilting during …

Large regions in which major late Cenozoic basin-range fault blocks are consistently tilted
are recognized in the western United States. The pattern of tilt domains is characterized by …

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 …

ABSTRACT The Basin and Range province covers a large region of western North America
and contains diverse late Cenozoic extensional structures, including metamorphic core …

In the Hebgen lake area of SW Montana, the Madison and South Fork Rivers occupy the
northeast sides of their respective meander‐belts. The form of the abandoned meander …

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

Abstract Changes in long profile, gradient, gradient index, pseudo-hypsometric integral,
valley incision, and sinuosity fractal dimension for rivers in western Oregon were studied to …

We use the landcape evolution model Zscape to explore quantitatively the development of
mountainous topography in the Basin and Range province (formerly the Basin Ranges) …

Repeated observations from the mouths of the Mississippi River from 1968 to 1973 indicate
that the relative contributions of outflow inertia, turbulence, bottom friction, buoyancy, and …