| BLOWOUT
Small, often circular or oval
depression in sand dunes, caused by wind scouring where protective
vegetation has been disturbed.
BLUFF
High, steep bank or cliff along
the mainland of non-coastal origin. Steepened bluffs are caused
by wave undercutting of the cliff toe.
BREAKWATER
Structure built parallel to
the shoreline and seaward of the beach designed to protect
the beach and upland areas by causing waves to break and dissipate
their energy before reaching the shore.
BUILDING
SETBACK State or locally required
seaward limit of beachfront construction, usually for a house.
BULKHEADS
Rigid structures with vertical
walls built parallel to the shoreline to serve as barriers
to wave attack and prevent storm surge flooding of upland
areas; constructed out of treated wood, corrugated steel,
PVC, or other materials.
COASTAL
COMPARTMENT Stretch of shore
that is connected by a common longshore sediment transport
system, such as the south shore of Long Island, New York.
CUSPS
Crenulated beach surface, characterized
by an evenly spaced series of rounded, small headlands (projections)
and bays (or embayments). The along-shore spacing of cusps
ranges from a few feet to 100s of feet and their relief
varies from a few inches to several feet.
DEFLATION
Lowering of the beach profile.
DOWNDRIFT
In the direction of net longshore
sediment transport.
DUNE
Mound or ridge of sand deposited
by the wind, capable of movement when unvegetated. Dune building
can be augmented by sand fencing or planting beach grass.
DUNE
RESTORATION Technique of rebuilding
an eroded or degraded dune through one or more methods (sand
fill, fencing, revegetation, etc.).
DUNE
WALKOVER Light construction
that provides pedestrian access across a dune without trampling
the vegetation.
EBB
CURRENT Tidal current moving
away from the coast during a falling (ebbing) tide, often
with high velocity flows through tidal inlets.
EBB
TIDAL DELTA Sandy shoals formed
by ebbing currents found on the seaward side of tidal inlets.
EROSION
Physical removal of sand from
the beach which is transported offshore, alongshore, or into
bays and lagoons via inlets. Erosion results in shoreline
recessionlandward retreat of a shoreline indicator such
as the high water line, vegetation line or dune line. Opposite
of accretion.
|