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- W2269884456 abstract "The fine (<62 um) fraction of New Jersey beach and inner shelf sediments is derived from both local and regional sources. Coastal and shoreface erosion released significant amounts of mineralogically distinguishable fine sediment into the nearshore zone. Fine clay (<0.5 um) is dominated by illite and kaolinite and/or chlorite, with lesser amounts of quartz and smectite. The heavy mineral fraction of silt-sized sediment (8-32 um) is dominated by hornblende and chlorite. North of Long Branch, fine clay is derived from erosion of glauconite-rich upper Cretaceous and early Tertiary coastal plain formations, and transported northward to Sandy Hook. The fine clay on the beaches and in the nearshore region of Cape May Peninsula is apparently derived from erosion of Cape Kay Formation (Pleistocene) clays, which probably crop out on the inner shelf and in Delaware Bay. These clays contain measurable amounts of smectite. Between Little Egg Inlet and Long Branch, beach and nearshore clays may receive some input from erosion of the kaolinite-rich Kirkwood and Cohansey Formations (Miocene). Hornblende-enriched silt is derived from the (Miocene?) Eridgeton Formation, and appears to be transported northward of its probable source area (little Egg Inlet to Cape May Peninsula). This transport pattern may result from summer and fall nearshore flow toward the northeast, which is opposite to the previously observed" @default.
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- W2269884456 date "1980-01-01" @default.
- W2269884456 modified "2023-09-27" @default.
- W2269884456 title "The mineralogy of fine-grained sediment in the New Jersey nearshore region: Implications for sediment sources and dispersal patterns." @default.
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