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The present knowledge of Holocene continental shelf deposits in relation to the processes for their formation, from the prospective of marine sediment dynamics, is examined. Over the last 50years, various innovative techniques have been developed to measure and calculate currents, waves and suspended sediment concentrations. Thus, sediment transport rates can be defined by in situ observations, or...
Geophysical surveys, current meter measurements and fluorescent sand tracer experiments were undertaken in the vicinity of the Broken Bank. The data are used to establish localised and regional patterns of water and sediment movement.The results obtained confirm mechanisms proposed previously for sandbank growth, with particular reference to the North Sea; these include the clockwise circulation...
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