For the Instructor
These student materials complement the Coastal Processes, Hazards and Society Instructor Materials. If you would like your students to have access to the student materials, we suggest you either point them at the Student Version which omits the framing pages with information designed for faculty (and this box). Or you can download these pages in several formats that you can include in your course website or local Learning Managment System. Learn more about using, modifying, and sharing InTeGrate teaching materials.Delta Morphologies and Driving Processes
Variations in delta morphology tell us something about the processes that cause and drive the evolution of deltaic environments. Globally it is widely accepted that there are three end member morphologies of deltas that reflect the relative influence of wave energy and tidal energy in the receiving basin or sediment input by the source river into the receiving basin. On a ternary plot, these three end members each represent one apex of the plot and all deltas fall somewhere on this plot (Figure 3.29). Deltas that are primarily the result of high rates of sediment input tend to be elongated because of their rapid outbuilding associated with high rates of deposition into the receiving basin (Figure 3.30). Wave influenced deltas have smooth, often arcuate shorelines with numerous ridges that reflect the longshore transport of river-delivered sediment by the high wave energy (Figure 3.31). Tidally influenced deltas have numerous shoreline perpendicular tidal passes and tributaries with sediment bodies aligned parallel to the direction of tidal exchange (Figure 3.32).
Credit: after Galloway, 1975
Credit: http://visibleearth.nasa.gov/view.php?id=8103; NASA image created by Jesse Allen, using data provided by the University of Maryland's Global Land Cover Facility.
Credit: NASA
Credit: NASA