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Even though our state's coastline
is only 187 miles long, 3000 miles of actual shoreline are created from
the various estuaries,
bays, rivers, and creeks (OCRM, 2000).
The location of these various bodies of water help to determine the distinct
shoreline types found along South Carolina’s coast.
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| Photo provided by www.myrtlebeachsites.com |
- The arcuate strand is a crescent-shaped beach
stretching from the North Carolina –South Carolina border south to Winyah
Bay, SC (OCRM, 2000). This area is generally considered the most stable
region along the S.C. coast. It is a wide, continuous beach approximately
60 miles long with few tidal inlets. The absence of inlets in this region
is also associated with the lack of barrier
islands and salt
marsh. Why? Inlets are waterways between barrier islands that transport
water to and from the estuaries and the ocean.
- The cuspate delta, south of the arcuate strand
between Winyah Bay and Bulls Bay, is referred to as the Santee River
Delta (OCRM, 2000). It is the largest deltaic complex located on the
eastern seaboard of the United States and is 18 miles long. Here, headlands
(or capes) extend into the ocean and form elongate spits.
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Photo provided by www.photolib.noaa.gov/
nerr/nerr0313.htm
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- The barrier island complex, south of Bulls Bay
to the Georgia border, includes transgressive
barrier islands and beach-ridge
barrier islands. These relatively thin, elongate islands are located
along the majority of South Carolina’s central and southern shoreline.
They protect our coastal areas from storm forces and rising sea level
(OCRM, 2000).
- Beach-ridge barrier islands (also referred
to as prograding barrier islands) are larger islands that contain
a beach, vegetated sand dunes, shrubs, and a maritime
forest. Kiawah Island is an example of this type of barrier
island.
| Photo provided by www.golfpac.com/.../ westin_hilton_head_resort.htm |
- Transgressive barrier islands are long,
narrow islands that are extremely unstable because they lack heavy
vegetation and healthy dune
systems (OCRM, 2000). These are referred to as retrograding
islands because they retreat landward. Folly
and Morris Islands are typical examples of this type of barrier
island and will be the focus of the CD-Rom.
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