Date of Award
Master of Science (MS)
Dennis A. Darby
John C. Ludwick
The Norfolk, Kempsville, and Sand Bridge Formations beneath the HIckory Scarp of southeastern Virginia are reinterpreted as representing one glacio-eustatic transgressive cycle. The timing of this transgressive event is set during the earliest Wisconsinan. The formations were previously interpreted as unconformable overlying one another. The Norfolk-Kempsville unconformity is actually a diagenetic boundary. Evidence is presented which indicates that the Kempsville Scarp area should be reduced to member status or dropped entirely.
Jasper, Alan K..
"Stratigraphy and Depositional Environments of a Late Pleistocene Barrier Island Complex, Southeastern Virginia"
(1982). Master of Science (MS), Thesis, Ocean/Earth/Atmos Sciences, Old Dominion University, DOI: 10.25777/bdtz-k987