The interplay between a meandering river and the changing sedimentary
environment created by the river itself, at earlier times during its d
evelopment, was studied using a computer simulation model. Our treatme
nt of the river migration is based directly on the bend-erosion theory
of Ikeda et al. In the present work, this well-known theory is augmen
ted by a sedimentation model intended to describe geological heterogen
eities and the evolution of these heterogeneities under the influence
of the river itself. The different forms of individual meanders observ
ed in various natural sedimentary environments have been reproduced by
the model. The long-term effects of meandering river evolution, inclu
ding the formation of a meander belt that restricts the lateral migrat
ion of the river, have also been explored using the model.