The beach is more than a space for people to walk, sunbath and swim. It has a past and a future  and this indicates  that  the sand dunes and the fragile dune  vegetation are in  need different forms of coastal protection and management.   Hence the use of both sand-drift fencing to help restore and protect dune systems from erosion, by trapping wind-blown sand in the vicinity of the fence where natural vegetation is not sufficient to do so effectively, and various  revegetation and restoration projects.

Beaches have a history and for Adelaide’s coastal beaches this history  is one of coastal degradation.

Prior to European settlement, the beaches were naturally replenished from the dunes and the southern beaches,  and therefore sand movement could continue almost indefinitely. Predominant wave energy hitting beaches from the southwest naturally shifted sand in a northerly direction along the coastline with most of the sand accumulating at Semaphore and North Haven. Development along our coast however, has resulted in large quantities of the sand supply either being ‘locked up’ (eg., ate the harbours at Glenelg and West Beach) or removed from the beach system, preventing natural replenishment.  As a result, natural processes and coastal storms have continually eroded beach width, and without artificial replenishment, the sand will continue to erode away, exposing the underlying hard rocks and clays.

One  future scenario is that the  ongoing beach erosion  will result in  the  beaches at Glenelg, Henley Beach and Semaphore  being all that remains of the metropolitan coast beyond 2026.The rest of the coastline will become a rocky foreshore, like Hallett Cove, and will be lined by rock walls. Ongoing sea level rise will make it more difficult to retain sand along the coast.This ‘movement of sand’ shifts about 70 000 m3 of sand northwards along the metropolitan coast every year. Unfortunately, the natural sand supply to the southern end of the metropolitan coast is only about 10 000 m3 per year. Without some form of artificial replenishment, the sand on the southern beaches would drift away.

The history is one in which the coastline south of Adelaide reflects the sorry chronology of decisions made in ignorance of the ecological functioning of coastal lands and waters. These decisions have lead to loss of sea grasses due to storm water discharge and sewerage pollutions; loss of beaches from impairment of normal tidal and wave action by inappropriate groins and marinas and from residential development on land created by bulldozing foreshore land over the top of sand dunes.