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all geography including DSDP/ODP Sites and Legs
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sedimentary rocks
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Abstract: Eleven tidal marsh stations along the lower Hudson River estuary yield contrasting marine transgression rates: more than 2.0 m/millennium at New York City compared to about 1.0 m/millennium 100 km to the north at Marlboro near Poughkeepsie. The entire area appears to be tilting downward to the south-southeast. Three tidal marsh stations within the Ramapo Fault Zone (RFZ) yield higher transgression rates as compared to the other stations beyond the limits of the RFZ. This anomaly seems best explained by complex graben-like downfaulting, with a throw of at least 1 m having occurred within the past 2 millennia. There is also evidence, based on radiocarbon dating, of earlier fault movement after about 4.2 ka, suggesting a recurrence interval on the order of 2,000 yrs. The displacements inferred from these varying transgression rates may result from faults whose traces do not intersect the earth's surface.