A plan view approach to the study of a beach has the advantage that the obvious requirement (map outline) can be met from maps and/or air photos. It has the disadvantage that the three-dimensional geometry, and time changes in that geometry are ignored. Nevertheless certain useful results can be obtained from a study of the plan view.
The Cell Concept
Along a sandy coast, the ideal cell can be defined as a single area of erosion, a single area of deposition, and the transport path between. Cells are bounded along the coast in various ways: rocky headlands, sandy capes, bay heads, wide inlets, estuary mouths, deltas, submarine canyons, marine marsh or swamp, and others. For two cells to be isolated from each other there must be little or no leakage of sand past their common boundary. In nature some cells are well isolated, and others are poorly isolated, commonly gaining or losing significant amounts of sand from or to adjacent cells; these last are better considered as subcells.
Maturit...
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Tanner, W.F. (1982). Beach in plan view . In: Beaches and Coastal Geology. Encyclopedia of Earth Sciences Series. Springer, New York, NY. https://doi.org/10.1007/0-387-30843-1_57
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