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• W2086674550 abstract "The Dornoch Firth area contains widespread evidence of Holocene relative sea-level changes. In this study, one and possibly three raised shorelines have been identified on the basis of morphological evidence and have been found to slope downwards towards the north. The highest of these raised shorelines, which reaches up to +7.2 m OD, is correlated with the Main Postglacial Shoreline in Scotland. Stratigraphical and palaeoecological studies of coastal sediment sequences, including radiocarbon dating, disclose a sequence of relative sea-level changes. This began with a fall in relative sea-level from a buried estuarine surface lying at c. −2.0 m OD shortly before c. 9600 bp. Subsequently, a rapid rise of about 7 m took place between c. 7900 and c. 7000 bp, following which, relative sea-level reached the highest raised shoreline. Shortly before the rise in relative sea-level culminated, at c. 7000 bp, a high-energy marine flood occurred. This flood is correlated with a tsunami thought to have occurred about this time in the Northern North Sea. The subsequent fall in relative sea-level to the present may not have been continuous." @default.
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• W2086674550 date "1992-01-01" @default.
• W2086674550 modified "2023-10-18" @default.
• W2086674550 title "Holocene relative sea-level changes and shoreline displacement in the Dornoch Firth area, Scotland" @default.
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• W2086674550 doi "https://doi.org/10.1016/s0016-7878(08)80232-5" @default.
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