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Hydrons and Alongshore Migrating Undulating Beach Forms

J. Ernest Breeding Jr.
The Journal of Geology
Vol. 89, No. 2 (Mar., 1981), pp. 260-265
Stable URL: http://www.jstor.org/stable/30078291
Page Count: 6
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Since scans are not currently available to screen readers, please contact JSTOR User Support for access. We'll provide a PDF copy for your screen reader.
Hydrons and Alongshore Migrating Undulating Beach Forms
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Abstract

A beach undulation (rhythmic topography) is an equilibrium beach form. The water wave energy flux depends upon the refraction of the hydrons (water wave packets), and the angle of the breaking waves is determined by the refraction of the wavelets within a hydron. The refraction of the hydrons and wavelets work together to provide a constant longshore drift of sediments.

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