|2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM|
|Paper No. 227-6|
|Presentation Time: 9:40 AM-9:55 AM|
Regional Coastal Evolution along the Mississippi River Delta Plain Barrier Shorelines
MINER, Michael D., Pontchartrain Institute for Environmental Sciences, University of New Orleans, 2000 Lakeshore Dr, New Orleans, LA 70148, firstname.lastname@example.org, KULP, Mark A., Dept. of Earth and Environmental Sciences, University of New Orleans, 2000 Lakeshore Drive, New Orleans, LA 70148, FLOCKS, James, Center for Coastal and Watershed Studies, U.S. Geol Survey, 600 4th Street South, St. Petersburg, FL 33701, TWICHELL, David C., U.S. Geol Survey, 384 Quissett Campus, Woods Hole Road, Woods Hole, MA 02543, FITZGERALD, Duncan, Boston University, Boston, MA 02215, and LEE, Darin, Office of Coastal Restoration and Management, Louisiana Department of Natural Resources, Thibodaux Field Office, 1440 Tiger Drive, Suite B, Thibodaux, LA 70301|
Data from regional bathymetric surveys conducted in 2006-2007 along Louisiana's South-Central and Chandeleur barrier shorelines were combined with historical bathymetry from three time periods (dating to the 1880's) to provide a series of digital elevation models that show the 3-D morphological evolution. Both areas are undergoing pronounced shoreface retreat due to rapid relative sea level rise and a net loss of sediment. The two regions have contrasting evolutions: tidal inlet processes dominate the central barriers, whereas hurricane impacts and subsequent storm recovery processes dominate the Chandeleur Islands.
Along the South-Central barriers, conversion of interior wetlands to open water increases tidal prism, resulting in degradation of barriers due to increasing inlet cross-sectional area and sediment sequestration in ebb tidal deltas. The dominant trends during the past 125 years include erosion of ~9x108m3 of sediment from the shoreface and an increase in combined tidal inlet cross-sectional area from ~41,400m2 to ~139,500m2. The rate at which tidal inlet cross-sectional area is increasing is directly proportional to the rate of interior wetland loss.
Along the Chandeleur Islands, long-term reduction in island area is event-driven and related to major storms. The islands do not fully recover from large magnitude hurricanes because storm waves transport sand away from the mid-barrier arc to the distal flanks of the system. Volume calculations indicate ~150x106m3 of sediment has been deposited downdrift and seaward of the northern terminal spit during the past 125 years, whereas approximately half this volume has been deposited in the backbarrier.
This study is refining coastal evolutionary models and management schemes for these regions by: 1. quantifying erosional trends in degrading delta complexes, 2. identifying linkages between interior wetland loss and barrier response, 3. documenting sediment sinks, and 4. demonstrating the importance of implementing a system-wide approach to sediment management in the Mississippi River delta plain.
2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM
General Information for this Meeting
|Session No. 227|
The Mississippi River Delta as a Natural Laboratory for Evaluating Coastal Response to Relative Sea-Level Rise and Innovations in Transgressive Coastal Management: Shea Penland Memorial Session
George R. Brown Convention Center: General Assembly Theater Hall A
8:00 AM-12:00 PM, Tuesday, 7 October 2008
Geological Society of America Abstracts with Programs, Vol. 40, No. 6, p. 314
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