ABSTRACT
Coastal, estuarine, fluvial and submarine morphodynamics encompass some of the leading processes shaping
our planet and stems mainly, but not only, from the interaction of water in motion and movable sediment
boundaries resulting in morphological changes produced by erosion, transport and deposition of sediments that
generate a variety of landscapes and seascapes over time. Morphodynamics allows for a better understanding
and interpretation of self adjustments in drainage basins, longitudinal river profiles and shorelines shapes, as
well as characteristic features such as beach cusps, bed forms such as dunes, and channel patterns.
