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A Socio-Economic Environmental Baseline Summary For The South Atlantic Region Between Cape Hatteras, North Carolina And Cape Canaveral, Florida Volume Iv: Geological Oceanography, Virginia Institute Of Marine Science
A Socio-Economic Environmental Baseline Summary For The South Atlantic Region Between Cape Hatteras, North Carolina And Cape Canaveral, Florida Volume Iv: Geological Oceanography, Virginia Institute Of Marine Science
Reports
The geographic area covered in this report extends from Cape Hatteras, North Carolina, on the north, to Cape Canaveral, Florida, to the south. Included within this area are portions of the coastal areas of South Carolina and Georgia. All or portions of thirty coastal counties are included within the study area.
- Chapter 1 - Introduction
- Chapter 2 - Coastal Plain-Subzone I-Cape Hatteras to Winyah Bay
- Chapter 3 - Coastal Plain-Subzone II-Winyah Bay to St. Johns River
- Chapter 4 - Coastal Plain-Subzone III-St. Johns River to Cape Canaveral
- Chapter 5 - Continental Shelf-Subzone I-Cape Hatteras to Winyah Bay
- Chapter 6 - …
Sediment Transport Processes In A Salt Marsh Drainage System, John Daniel Boon Iii
Sediment Transport Processes In A Salt Marsh Drainage System, John Daniel Boon Iii
Dissertations, Theses, and Masters Projects
No abstract provided.
Mechanics Of Beach Cusp Formation, Asbury H. Sallenger
Mechanics Of Beach Cusp Formation, Asbury H. Sallenger
Dissertations, Theses, and Masters Projects
Beach cusps are crescentic shoreline accumulations of unconsolidated sediment that are characterized by a quasi-equal longshore spacing. The processes controlling the development of the cuspate form and the spacing of cusps were investigated. Field measurements showed that the cuspate form was derived through erosion of beach ridges, The ridges oriented alongshore in the swash zone are characterized by quasi-equally spaced channels cut normal to the shoreline whose widths are much less than the channel spacing. The upwash flows up the front face of the ridge and ponds shoreward of the ridge crest. The ponded fluid returns seaward through the channels. …
Carbon Transport In Two York River, Virginia Tidal Marshes, Kenneth Alan Moore
Carbon Transport In Two York River, Virginia Tidal Marshes, Kenneth Alan Moore
Dissertations, Theses, and Masters Projects
Annual net transports of particulate organic carbon (POC), dissolved organic carbon (DOC), and ATP-carbon were determined for two York River, Virginia, tidal marshes by monthly sampling for one year. Annual net losses of POC, DOC, and ATP-carbon from the marsh to the York River were observed for both areas, indicating that the long-term effect of these marshlands is to contribute both living and detrital organic material to the estuary. The mesohaline marsh area, Carter Creek, was observed to have the greater amount of organic carbon loss in the particulate fraction, while the oligohaline marsh area, Ware Creek, was observed to …