This document discusses fluvial depositional models and uses the Late Triassic Chinle Formation in Petrified Forest National Park as a case study. It finds that the Chinle Formation represents a distributary fluvial system rather than a tributary one. As subsidence decreased over time, the fluvial system prograded in a coarsening upward sequence. Paleosol changes reflected relative elevation to the water table rather than changes in aridity. Both tributary and distributary fluvial systems should be considered when interpreting continental strata.