A climate of arctic severity prevailed in Britain throughout much
of the last two million years, resulting in the widespread
formation of a great range of periglacial landforms and deposits.
Many of these features provide key evidence for understanding the
evolution of the present landscape and reconstructing former
climate. Appreciation of the significance of periglacial deposits
and structures is also important in many engineering operations and
in understanding the development of present-day soils. This book,
first published in 1994, provides a synthesis of theory in
periglacial geomorphology and applies this to the study of
periglacial phenomena in Great Britain. The first part of the book
introduces the chronological and environmental background to
periglaciation in Britain. The second and third parts deal
respectively with the periglaciation of lowland Britain and upland
Britain. The book concludes by considering the implications of
periglacial phenomena for environmental reconstruction.
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