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- W3193816096 abstract "Substantial beach and dune complexes have formed along the east coast of Scotland particularly, within St Andrews Bay, Montrose Bay, Aberdeen Bay and Belhaven Bay, where the interplay of relative sea-level change and availability of glacial and paraglacial sediment sources has locally favoured sand and gravel accumulation since the mid-Holocene. Most of these complexes began to develop when sea level was higher and sediment supply abundant, but have since merged, often imperceptibly, into younger and modern features at present sea level. Some substantial dune systems have now stabilised into fixed parabolic dune forms, whilst others remain highly active and mobile. In locations, where local factors have offset an overall decline in the availability of beach-building sediments, coastal accretion has continued, albeit supplied from the ongoing erosion of beaches and dunes elsewhere. Beach and dune development in eastern Scotland can be understood in the context of discrete coastal sediment cells, with boundaries generally formed by prominent headlands, a context likely to have been in place over much of the Holocene." @default.
- W3193816096 created "2021-08-30" @default.
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- W3193816096 date "2021-01-01" @default.
- W3193816096 modified "2023-09-23" @default.
- W3193816096 title "Beaches and Dunes of Eastern Scotland" @default.
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- W3193816096 doi "https://doi.org/10.1007/978-3-030-71246-4_23" @default.
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