The University of Sheffield
Department of Geography

Cryostratigraphy of aeolian sand sheets in arctic Canada and NW Europe

During much of the Quaternary, NW Europe experienced cold, non-glacial conditions. A legacy of these periods are the periglacial structures found in the stratigraphic record, many of which contain wind-blown material. Unfortunately, the reconstruction of the conditions responsible for these features has been hindered both by a limited understanding of cryogenic processes and structures, and by the fragmentary nature of terrestrial Quaternary sequences.

Recent progress in understanding contemporary features indicates that the cryostratigraphical record may hold key information on the rates of climatic amelioration. Investigations are currently being carried out to date and characterise such structures in Arctic Canada and relate them to relict evidence in NW Europe.

The work is partly funded by The Royal Society and NERC. Ten publications and one further one in press have come from this work so far.

Key Outcomes

Lake Aggassiz


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Hadwen Island, Canada


Recent papers