Longshore drift is the gradual movement of beach materials such as sand and shingle along a shore. This process is the result of waves breaking at an angle on to a beach: driven by obliquely breaking waves, a thin layer of turbulent water known as the swash moves diagonally up the beach, carrying sand and shingle landward and depositing them when it runs out of energy. Some of this material is then carried back down into the breaker zone by the returning backwash. The net effect is that material is moved in small steps sideways along the beach, a process which may be aided by longshore currents.
Longshore drift may result in extensive beach erosion, the material removed being ultimately redeposited further down the coast. In some seaside areas attempts have been made to stop such erosion by erecting groynes, man-made barriers which extend down the beach and into the sea, and behind which sand and shingle moving along the shoreline are trapped. Research Longshore Drift
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Research Longshore Drift