A three-dimensional model of alluvial stratigraphy has been developed to simulate the
spatial distribution, proportion, and connectedness of coarse-grained channel-belt deposits …

The quantitative model presented simulates the development of a two‐dimensional alluvial
sedimentary succession beneath a floodplain traversed by a single major river. Several inter …

Quantitative models of alluvial stratigraphy have been widely used to interpret the
architecture of ancient alluvium. However, with few exceptions, these interpretations have …

In an extended series of papers by M. Leeder, JRL Allen, JS Bridge, J. Alexander, and
others, the depositional stacking patterns of channel-belt deposits were related to tectonic …

The geometry and distribution of channel‐belt sandstone bodies in alluvial deposits have
been simulated recently using stochastic models. These models are based on Monte Carlo …

Various, but related, models have been proposed to explain the architectural arrangement of
channel stacking patterns in avulsion-dominated alluvial sequences. The early models …

Floodplain paleosols in time-equivalent strata of the Willwood For mation differ in terms of
paleodrainage and degree of pedogenic development. Ancient soils were more poorly …

River avulsions are commonly considered to be driven by the aggradation and growth of
alluvial ridges, and the associated increase in cross‐valley slope relative to either the down …

Present models of river sedimentation are based largely on a classification of the
geomorphology of present‐day river channel patterns. The classes are difficult to apply with …

The fluvial system is a major concern in modeling landform evolution in response to tectonic
deformation. Three stream bed types (bedrock, coarse‐bed alluvial, and fine‐bed alluvial) …