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The volume of reservoir quality sand was estimated from barrier islands, ebb tidal deltas, sand flats, tidal point bars, and tidal sand ridges along the South Carolina coast.

(46) Shadroui, J. M. 1990. Aeolian transport in a small dune field on St. Catherines Island, Georgia. Bulletin of the Georgia Geologic Society, 122:48-64.

Sand dunes on St. Catherines Island, Georgia were monitored for 15 months in order to describe erosion and accretion patterns.

(47) Stallins, J.A. 2000. Barrier island morphology and dune vegetation pattern and process in the Georgia bight. PhD Dissertation (Abstract ), University of Georgia, Athens.

This study examines how vegetation and disturbance are related on two barrier islands: South Core Banks, North Carolina and Sapelo Island, Georgia.

(48) Stapor, F.W. and T.D. Mathews. 1983. Higher than present Holocene sea-level events recorded in wave cut terraces and scarps: Old Island, Beaufort County, South Carolina. Marine Geology, 52:M53-M60.

Wave cut terraces and scarps around Old Island, South Carolina were used to show at least two higher than present Holocene sea level events.

(49) Sullivan, J.D. 1988. Late Pleistocene – Holocene Transgressive Barrier Island Sequence: Evidence for a Fluctuating Sea Level, Hilton Head Island Area, South Carolina. Masters Thesis. Georgia State University, Atlanta.

Stratigraphic analysis of Hilton Head Island, South Carolina supports other evidence suggesting sea level fluctuations over the past 7000 years.

(50) Swanson, V.E. and J.G. Palacas. 1965. Humate in coastal sands of northwest Florida. U.S. Geological Survey, Bulletin 1214B. 27 p.

Layers of dune and beach sand impregnated and cemented with organic material are discussed in terms of their formation processes.

(51) Thom, B.G. 1967. Humate and Coastal Geomorphology. Louisiana State University Coastal Studies Series, Bulletin 1.


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