Storm large dating

Until recently, prehistoric hurricanes and their intensity levels have been automatically interpreted from the frequency and thickness of sand layers in muddy paralic deposits.

However, in addition to wind velocity, several hydro-, aerodynamic, and other factors a wide range of stratigraphic conditions, topographic setting, and sand sources also determine variations in the extent and intensity of storm flooding, erosion, transfer, and deposition of sand layers in small paralic basins.

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Detection and documentation of hurricane signatures in coastal deposits are becoming instrumental in attempts to reconstruct mid and late Holocene storm climate history.

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Storm events can also have dramatic results on adjacent rock coastlines, with storm boulder ridges emplaced by large waves, burying sand deposits on cliff-top sites.

Work has been undertaken using a quartz SAR protocol to date sand deposition at two archaeological sites in Orkney and a cliff-top site in Shetland.

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