What is a wave-dominated coast?

Abstract During the past decade or so, various coasts have been designated as wave-dominated or tide-dominated. Typically there is an association made between coastal morphology and the dominant process that operates on the coast in question. Most authors consider long, smooth, barrier coasts with few inlets and poorly developed ebb deltas as “wave-dominated”. These coasts are associated with microtidal ranges. Conversely, mesotidal coasts tend to develop short, drumstick-shaped barriers with well-developed ebb deltas. They are considered as tide-dominated barriers. Such generalizations may be restricted to coasts with moderate wave energy although this is commonly not stated. Exceptions to these stated generalizations are so numerous that wave energy and tidal prism must also be included in characterizing coasts. The relative effects of waves and tides are of extreme importance. It is possible to have wave-dominated coasts with virtually any tidal range and it is likewise possible to have tide-dominated coasts even with very small ranges. The overprint of tidal prism will also produce tide-dominated morphology on coasts with microtidal ranges.

[1]  G. Evans Intertidal flat sediments and their environments of deposition in the Wash , 1965, Quarterly Journal of the Geological Society of London.

[2]  Richard A. Davis,et al.  Hydrodynamics and sedimentation in wave-dominated coastal environments , 1984 .

[3]  P. Allen Wave‐generated structures in the Devonian lacustrine sediments of south‐east Shetland and ancient wave conditions , 1981 .

[4]  K. Clayton,et al.  Geographical variation in coastal development , 1972 .

[5]  G. Klein A Sedimentary Model for Determining Paleotidal Range , 1971 .

[6]  G. Evans Intertidal Flat Deposits of the Wash, Western Margin of the North Sea , 1975 .

[7]  W. F. Tanner Florida Coastal Classification , 1960 .

[8]  A. Heward A review of wave-dominated clastic shoreline deposits , 1981 .

[9]  J. Kraft Sedimentary Facies Patterns and Geologic History of a Holocene Marine Transgression , 1971 .

[10]  J. Glaeser Global Distribution of Barrier Islands in Terms of Tectonic Setting , 1978, The Journal of Geology.

[11]  H. N. Fisk Padre Island and the Laguna Madre Flats, Coastal South Texas , 1959 .

[12]  J. M. Coleman,et al.  Physical Processes and Fine-grained Sediment Dynamics, Coast of Surinam, South America , 1981 .

[13]  M. C. Davies,et al.  A morphogenic approach to world shorelines , 1964 .

[14]  P. Komar Oscillatory ripple marks and the evaluation of ancient wave conditions and environments , 1974 .

[15]  R. Dalrymple,et al.  Intertidal Sediments from the South Shore of Cobequid Bay, Bay of Fundy, Nova Scotia, Canada , 1975 .

[16]  William E. Galloway,et al.  Process Framework for Describing the Morphologic and Stratigraphic Evolution of Deltaic Depositional Systems , 1975 .