Base‐level changes occur over a broad range of time‐scales and may result from several
interacting factors. As a result, relative sea‐level has changed considerably over geological …

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

Results obtained during 20 yr of experimental research at Colorado State University (CSU)
provide partial answers to questions posed by the conveners of this symposium on the …

A river crossing a coastal plain is assigned a zone of influence within which it may abruptly
move and construct new channel sand-bodies following avulsion. Assuming uniform and …

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 …

The alluvial stratigraphy model of Bridge and Leeder [A simulation model of alluvial
stratigraphy: Sedimentology, v. 26, no. 5, p. 617–644 (1979)] has been improved to simulate …

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

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 …

A model to simulate the development of a two-dimensional alluvial sedimentary succession
beneath a floodplain traversed by a single major river is described briefly; account is taken …

The two-dimensional alluvial stratigraphy model of Bridge and Leeder (1979) has been
improved to more accurately simulate alluvial depositional processes and to predict the …