Abstract: Historical shoreline and bathymetric survey data were compiled for the barrier islands and passes fronting Mississippi Sound to develop a regional sediment budget spanning a 90-year period. Net littoral sand transport along the islands and passes is primarily unidirectional (east-to-west). Beach erosion along the east side of each island and sand spit deposition to the west result in an average sand flux of about 430,000 cy/yr throughout the barrier island system. Dog Keys Pass, located updrift of East Ship Island, is the only inlet that is a net sediment sink. It also is the widest pass in the system and has two active channels and ebb shoals. As such, a deficit of sand exists along East Ship Island. Littoral sand transport decre...
The Mississippi-Alabama barrier islands restrict exchange between the Mississippi Sound and Mississi...
The majority of changes to barrier island shorelines can be attributed to tidal inlet processes, and...
Although Mississippi's toehold on the Gulf of Mexico extends less than 110 km from border to border ...
In order to conceive any realistic plan for post-Katrina island restoration, it is necessary to unde...
The shorefront and nearshore waters of Harrison County, Mississippi, have been extensively modified ...
Basic differences between non-deltaic regressive and deltaic transgressive barrier islands reflect m...
A wealth of new data provides a well-constrained chronology of mid- to late Holocene coastal develop...
© 2020 Elsevier B.V. Horn Island, one of the two most stable barriers along the Mississippi-Alabama ...
Rapid land loss in the Mississippi River Delta Plain has led to intensive efforts by state and feder...
Recent reports estimate that the marshes of the Mississippi Delta receive just 30% of the sediment n...
Deltas worldwide share the same sinking problem in face of pressure from natural and anthropogenic a...
A shoreline change analysis was performed along the shoreline of the chenier plain in southwestern L...
This report is preliminary and has not been edited or reviewed for conformity with Geological Survey...
Abstract: The 133-km barrier island chain extending east from Fire Island Inlet to Montauk Point, N...
A geologic investigation was conducted in Mississippi Sound to determine patterns of estuarine sedim...
The Mississippi-Alabama barrier islands restrict exchange between the Mississippi Sound and Mississi...
The majority of changes to barrier island shorelines can be attributed to tidal inlet processes, and...
Although Mississippi's toehold on the Gulf of Mexico extends less than 110 km from border to border ...
In order to conceive any realistic plan for post-Katrina island restoration, it is necessary to unde...
The shorefront and nearshore waters of Harrison County, Mississippi, have been extensively modified ...
Basic differences between non-deltaic regressive and deltaic transgressive barrier islands reflect m...
A wealth of new data provides a well-constrained chronology of mid- to late Holocene coastal develop...
© 2020 Elsevier B.V. Horn Island, one of the two most stable barriers along the Mississippi-Alabama ...
Rapid land loss in the Mississippi River Delta Plain has led to intensive efforts by state and feder...
Recent reports estimate that the marshes of the Mississippi Delta receive just 30% of the sediment n...
Deltas worldwide share the same sinking problem in face of pressure from natural and anthropogenic a...
A shoreline change analysis was performed along the shoreline of the chenier plain in southwestern L...
This report is preliminary and has not been edited or reviewed for conformity with Geological Survey...
Abstract: The 133-km barrier island chain extending east from Fire Island Inlet to Montauk Point, N...
A geologic investigation was conducted in Mississippi Sound to determine patterns of estuarine sedim...
The Mississippi-Alabama barrier islands restrict exchange between the Mississippi Sound and Mississi...
The majority of changes to barrier island shorelines can be attributed to tidal inlet processes, and...
Although Mississippi's toehold on the Gulf of Mexico extends less than 110 km from border to border ...