Abstract

Abstract Detailed analyses and radiocarbon dating of buried soils have determined the characteristics and age of coastal aeolian sand deposits at Portstewart, Northern Ireland. A buried gleyed soil developed in basalt‐rich sandy loam underlies the sands. Two sand units occur, the lower of which contains a buried humus podzol 1.4 m thick. Radiocarbon dating indicates that this sand was deposited several hundred years after the mid‐Flandrian sea level maximum and that a long period (c. 4,300 years) of land‐surface stability occurred at the site. The upper sand unit was deposited in the late Middle Ages but its significance is not clear.

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