Short-Term Evolution of Cape Morphology: Cape Lookout and Cape Fear, North Carolina

dc.contributor.advisorDr. Tom Drake, Committee Chairen_US
dc.contributor.advisorDr. Jesse McNinch, Committee Memberen_US
dc.contributor.advisorDr. John Wells, Committee Memberen_US
dc.contributor.advisorDr. Lonnie Leithold, Committee Memberen_US
dc.contributor.authorBernstein, David Jerolden_US
dc.date.accessioned2010-04-02T18:01:02Z
dc.date.available2010-04-02T18:01:02Z
dc.date.issued2002-11-21en_US
dc.degree.disciplineMarine, Earth and Atmospheric Sciencesen_US
dc.degree.levelthesisen_US
dc.degree.nameMSen_US
dc.description.abstractCuspate forelands often occur as a series of seaward projecting capes and their cape-associated shoals. Capes are important physical and ecological discontinuities in a coastline, yet their dynamics are poorly understood. The barrier coastline of North Carolina, consisting of Capes Hatteras, Lookout and Fear, typifies a cuspate foreland coastline. The evolution and morphology of the subaerial cape points at Cape Lookout and Cape Fear, North Carolina were examined through a field-intensive study using Real-Time-Kinematic Global Positioning System (RTK-GPS) from September 2000 to August 2001. Topographic surveys of the subaerial cape points were conducted to assess changes in volume and shoreline position. Direct observation of waves, currents and bathymetry on cape-associated shoals is extremely difficult and often hazardous. This field-intensive study at Cape Lookout and Cape Fear uses the changing geometry of the subaerial cape point as an easily observed proxy for complex nearshore sediment transport processes at capes. Geo-spatial analysis of topography and shoreline position was used to assess geomorphic trends in volume change and shoreline variability. These results indicate that: 1) Short-term and seasonal changes in shoreline position are a result of changes in nearshore wind and wave energy; 2) variability in shoreline position and morphology increases with distance from the landward end of the cape to the seaward tip; and 3) the seaward tip of the subaerial cape point responds uniquely to changes in the nearshore wind and wave energy, and indicates that this region of the cape point plays a key role in sediment exchange between the subaerial cape and cape-associated shoal. Given the unique behavior of the seaward portion and transitional area of these capes, a previously un-described sequence of morphologic events I call 'clipping' plays a dominant role in the transfer of sand from the tip of the subaerial cape point offshore to the adjacent shoals.en_US
dc.identifier.otheretd-11202002-160539en_US
dc.identifier.urihttp://www.lib.ncsu.edu/resolver/1840.16/1131
dc.rightsI hereby certify that, if appropriate, I have obtained and attached hereto a written permission statement from the owner(s) of each third party copyrighted matter to be included in my thesis, dissertation, or project report, allowing distribution as specified below. I certify that the version I submitted is the same as that approved by my advisory committee. I hereby grant to NC State University or its agents the non-exclusive license to archive and make accessible, under the conditions specified below, my thesis, dissertation, or project report in whole or in part in all forms of media, now or hereafter known. I retain all other ownership rights to the copyright of the thesis, dissertation or project report. I also retain the right to use in future works (such as articles or books) all or part of this thesis, dissertation, or project report.en_US
dc.subjectErosionen_US
dc.subjectBeach Morpologyen_US
dc.subjectCuspate Forelanden_US
dc.subjectCape Fearen_US
dc.subjectCape Lookouten_US
dc.subjectRTK-GPSen_US
dc.subjectAccretionen_US
dc.titleShort-Term Evolution of Cape Morphology: Cape Lookout and Cape Fear, North Carolinaen_US

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