I suppose the beach owes some of its character to Dana Point itself, which influences both the shape of this coastline and the southward movement of sediment. The back of the beach is largely buried under the riprap revetment, which sort of limits the use of this beach to lower tides.
As with many other developments in California, there has been a long battle over public access on this site. A trail has been built along the top of the revetment (which allows people to walk where there was once a beach) and there are several public pathways that provide access from the public park at the top of the bluff.
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