INFLUENCES OF UNDERLYING GEOLOGY ON NEARSHORE AND SHORELINE PROCESSES

Jesse E. McNinch, Virginia Institute of Marine Sciences, School of Marine Science, The College of William and Mary, Post Office Box 1346, Gloucester Point, VA 23062-1346 and Thomas G. Drake, Department of Marine, Earth and Atmospheric Sciences, NC State Univ, 1125 Jordan Hall, NCSU Box 8208, Raleigh, NC 27695-8208.

Improved nearshore mapping techniques reveal locations along relatively straight, uniform beaches that have significantly different rates of erosion and accretion than surrounding areas and pose problems for beach nourishment. Such "hotspots" are usually associated with anomalous nearshore bar behavior and often recur year after year. Hotspots are thought to be correlated with variations in underlying coastal geology but the physical mechanism(s) responsible for coupling shoreline changes with shoreface geology remains speculative. Because hotspots occur in the shallow, energetic surf zone and evolve most rapidly during and immediately after storms when access to the surf zone is difficult, traditional methods of observation poorly document hotspots and give little insight into mechanisms for their creation and evolution. Recognizing the need for observing frequent, rapid and highly three-dimensional changes in sediment type, thickness, and bar morphology in the surf zone, we collected swath bathymetry, sidescan and Chirp seismic sub-bottom profiles from an amphibious vessel.

Our findings provide strong circumstantial evidence that a non-sandy underlying substrate present near the seafloor surface influences bar behavior and ultimately beach erosion and accretion. Eight surveys of a hotspot at Duck, North Carolina carried out over the last two years reveal a highly variable surface sand layer thickness and outcropping muddy substrates associated with anomalous nearshore bar behavior. Surface sediment samples and vibracores collected in conjunction with the surveys confirm that isolated and ephemeral spots of mud and gravel are exposed in the surf zone. Hourly ARGUS video imagery shows the shoreline closest to the outcrops and irregular nearshore bars has a much higher variance in erosion and accretion than the adjacent shoreline. We hypothesize that exposure of a non-sandy substrate across the surf zone inhibits the development and perturbs the usual migration patterns of nearshore bars which, in turn, changes the wave energy affecting the adjacent beach.

Supported by the Army Research Office and the National Research Council.


Abstract ID#: 4493
Password: 353372
Meeting: Southeastern Section - 50th Annual Meeting (April 5-6, 2001)
Session Type: Symposium
Selection: Beach Nourishment: The Wave of the Future for Erosion Control
Title: INFLUENCES OF UNDERLYING GEOLOGY ON NEARSHORE AND SHORELINE PROCESSES
Key Words: hotspot, nourishment, bathymetry
Presentation Format: Oral
Discipline Categories: Marine/Coastal Science

First Author

Presenting
Jesse E. McNinch
Virginia Institute of Marine Sciences, School of Marine Science, The College of William and Mary
Post Office Box 1346
Gloucester Point, VA 23062-1346
Office Phone: 804 684-7191
Email: mcninch@vims.edu

Second Author

Thomas G. Drake
Department of Marine, Earth and Atmospheric Sciences, NC State Univ
1125 Jordan Hall, NCSU Box 8208
Raleigh, NC 27695-8208
Email: drake@ncsu.edu