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- W2064857458 abstract "The existence of contiguous stretches of shoreline exhibiting erosion and accretion along the section of the East Anglian coast between Dunwich and Thorpeness cannot be explained in terms of normal processes of beach drifting by dominant waves. The influence of the offshore zone seems critical and for this area would appear to play a dual role. In the south, where a sediment bridge exists between the offshore Sizewell Bank and the coast at Thorpeness, the onshore transfer of sediment has helped to maintain the ness feature and given it a stability of position which is not apparent for other similar nesses along the East Anglian coast. The coastline at Dunwich stands out in marked contrast to the aggrading shoreline at Thorpeness for it has a long history or erosion. This is mainly due to a lack of an assured offshore supply to the beach. The marked drop in the rate of the erosion of the cliff face during the past fifty years coincides with a reduction in wave energy on the Dunwich shoreline as Sizewell Bank has grown steadily to the north." @default.
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- W2064857458 date "1980-08-01" @default.
- W2064857458 modified "2023-09-25" @default.
- W2064857458 title "Erosion and accretion along part of the Suffolk coast of East Anglia, England" @default.
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- W2064857458 doi "https://doi.org/10.1016/0025-3227(80)90014-6" @default.
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