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The AAPG/Datapages Combined Publications Database

Journal of Sedimentary Research (SEPM)

Abstract


Journal of Sedimentary Petrology
Vol. 42 (1972)No. 3. (September), Pages 596-601

Tidal Current Control of Sediment Distribution in Northumberland Strait, Maritime Provinces

Kate Kranck

ABSTRACT

In Northumberland Strait muddy sediments are being deposited in areas with maximum tidal current speeds (amplitude of M2) of less than 0.5 knots while sands and gravels occur in areas where currents are stronger than this. There is a direct relationship between the median diameter of bottom sediments and maximum tidal current speeds. Tidal current asymmetries occur such that the speed and duration of the ebb and flood currents differ. Two types of asymmetries are distinguished: Langrangian and Eulerian. Tidal current asymmetries and the presence of a residual current cause a difference in the amount of sediment transported in the ebb and in the flood direction and hence a net sdiment transport.


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