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• W2282364257 abstract "The heavy mineralogy of the New Jersey beach sands shows abrupt along-the-coast changes resulting in three mineralogical zones; zone 1 (Brigantine Inlet to Cape May Inlet); zone 2 (Barnegat Inlet to Brigantine Inlet and Cape May Inlet to, and including, the Delaware Bay shore); and zone 3 (Sandy Hook to Barnegat Inlet). Factor analysis results indicate that zone 1 sands are relatively rich in hornblende and hypersthene, zone 2 sands contain a relatively high percentage of black opaque minerals and tourmaline, and zone 3 sands are characterized by relatively large quantities of glauconite and collophane. The immediate source for the sand of zone 3 beaches, and the beaches of Cape May and the Delaware Bay shore is the coastal formations (Cohansey, Kirkwood, Cape May) which are subject to wave attack. South of Barnegat Inlet to Cape May Inlet the beaches are separated from the mainland by a lagoon complex. These barrier beaches are supplied exclusively with sand from the continental shelf, na indicated by analysis of the adjacent shelf sands. The abrupt change in mineralogy at Brigantine Inlet is npparencly due to different sources of sand on the shelf rather than selective sorting by longshore transport. These two distinct shelf sand sources reflect Pleistocene fluvial deposits on the New Jersey coastal plain/continental shelf." @default.
• W2282364257 created "2016-06-24" @default.
• W2282364257 creator A5014313970 @default.
• W2282364257 date "1982-01-01" @default.
• W2282364257 modified "2023-09-27" @default.
• W2282364257 title "Determination of the immediate source areas and probable sediment transport pathways of New Jersey beach sands." @default.
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