Abstract
Dunes and eolian cover sands play an important role in the morphology of Wolin Island and the surrounding area. From radiocarbon dates, palynological data, archaeological evidence and the study of Swedish maps from 1694, it can be inferred that the above forms accumulated in the Late Vistulian (Older Dryas and Younger Dryas) and Holocene periods, mostly in the Subboreal and Sub‐Atlantic periods. The development of eolian processes was due to climatic conditions during the Late Vistulian as well as the Holocene human involvement in the environment of dune‐covered areas and the absence of a vegetation cover on sand spits emerging successively from the sea.
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