Date of Award
Fall 1973
Document Type
Thesis
Degree Name
Master of Science (MS)
Department
Ocean & Earth Sciences
Committee Director
Donald J. P. Swift
Committee Member
Stanley R. Riggs
Committee Member
Gary Copeland
Committee Member
John C. Ludwick
Call Number for Print
Special Collections LD4331.O35S42
Abstract
The evolution of Platt Shoals, a complex ridge and trough system on the south side of the Albemarle Shelf Valley, was determined and the modern hydraulic regime was inferred. The methods used were surficial grain size, 11 vibracores, seismic profiling and bathymetric maps. Platt Shoals developed in a three step process. The first, step was the formation of a substrate of late Pleistocene regressive deposits from 15,000 to 30,000 yr B. P. The second step, occurring approximately 11,000 yr B. P., was the formation of estuary mouth shoals of the ancestral Albemarle River. Between 4,4.00 to 5,000 yr B. P., the estuary mouth was sealed and Platt Shoals was remolded by the modern shelf hydraulic regime which caused sand accretion on the ridge crests and erosion of the troughs. During the past one hundred years approximately 54,800 ft3 of sediment have been deposited on the ridges and 4.2,000 ft3 nave been eroded from the troughs. The modern hydraulic regime is inferred to consist of long quiescent periods and occasional storms which generate strong predominately south flowing currents that are channeled into the troughs and obliquely over the ridge crests.
Rights
In Copyright. URI: http://rightsstatements.org/vocab/InC/1.0/ This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
DOI
10.25777/gehy-xr31
Recommended Citation
Sears, Philip C..
"Evolution of Platt Shoals Northern North Carolina Shelf: Inferences from Areal Geology"
(1973). Master of Science (MS), Thesis, Ocean & Earth Sciences, Old Dominion University, DOI: 10.25777/gehy-xr31
https://digitalcommons.odu.edu/oeas_etds/293