Coversand deposits are prevalent across much of central and eastern contine
ntal Europe as distinct sedimentary units, but in comparison UK coversands
are fragmented and relatively thin. Arguably the best exposures of UK cover
sands are to be found in northern Lincolnshire, west of the Lincolnshire We
lds, where there are extensive coversand deposits up to 7 m thick. Stratigr
aphic, sedimentological, geomorphological and biological evidence show that
the Lincolnshire coversand is composed predominantly of a cold climate aeo
lian sandsheet. The same evidence also indicates provenance and westerly pa
laeowinds associated with coversand deposition. For the first time, through
the application of both thermoluminescence and radiocarbon dating, a good
chronological framework for coversand deposition in Lincolnshire has been e
stablished. This shows the main phase of coversand deposition took place be
tween c. 12,500 to 11,400 calendar years ago during the Younger Dryas clima
tic oscillation. The north Lincolnshire coversands are therefore contempora
ry with the Younger Coversands found in The Netherlands and Denmark. (C) 19
98 John Wiley & Sons, Ltd.