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Beaches
on the Georgia barrier islands are broad and gently sloping, just
as the Continental Shelf along the Georgia coast is broad and gently
sloping. Wave energy is low except during storms such as nor’easters
and hurricanes. Above the high-tide line, dunes develop when windblown
sand builds up behind small obstacles such as wrack, culms of dead
Spartina alterniflora washed out of the marshes and sounds
and deposited on the beach. Beach sand is constantly being eroded
and deposited and moved along the coast by tides, wind and long-shore
currents. This is known as the sand-sharing system.
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A
schematic cross-section through a Georgia barrier island shows the
relationship of the shifting dunes nearest the beachfront, the stable
dunes and the maritime forest and salt marsh which they protect from
the direct force of breaking waves. Once an obstacle has begun to
capture sand, the dune continues to grow unless high tides or storm
tides wash it away. Salt-tolerant foredune plants quickly begin to
colonize the new dune, and their roots are important factors in its
stabilization. Sea
oats, Uniola paniculata, is the most important of
these plants because of the depth of penetration and lateral spreading
of its root systems. Dunes along the Georgia coast often get as high
as 3 - 4 m. Even when they have been well-vegetated with sea oats
and other species they remain fragile and easily damaged by natural
forces as well as by man.
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Dune
Plants
Animals
on the Beach
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