The continuous agitation of the sea floor in the upper shoreface environment results in sediments that are winnowed of the smallest grains, leaving only those grains heavy enough that the water cannot keep them suspended. [1]
Depth of influence
Seawater is moved in a vertical circular motion when a wave passes. The radius of the circle of motion for any given water molecule decreases with depth.
The maximum depth of influence of a water wave is half the wavelength. Below that depth the water remains stationary as the wave passes.
For instance, in a pool of water 1 foot (0.30 m) deep, a wave with a wavelength of 1 foot (0.30 m) would not be able to cause water movement on the bottom. However, a wave with a 2 feet (0.61 m) wavelength would be moving the water (barely) at the bottom.
^ abR. G. Dean and R. A. Dalrymple (1991). Water wave mechanics for engineers and scientists. Advanced Series on Ocean Engineering. Vol. 2. World Scientific, Singapore. ISBN978-981-02-0420-4.
