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Extent of the last ice sheet in northern Scotland tested with cosmogenic 10 Be exposure ages

William M. Phillips; Adrian M. Hall; Colin K. Ballantyne; Steven Binnie; Peter W. Kubik; Stewart Freeman
Journal of Quaternary Science · Vol. 23, Issue 2 · pp. 101-107 · 2008

Abstract

The extent of the last British–Irish Ice Sheet (BIIS) in northern Scotland is disputed. A restricted ice sheet model holds that at the global Last Glacial Maximum (LGM; ca. 23–19 ka) the BIIS terminated on land in northern Scotland, leaving Buchan, Caithness and the Orkney Islands ice‐free. An alternative model implies that these three areas were ice‐covered at the LGM, with the BIIS extending offshore onto the adjacent shelves. We test the two models using cosmogenic 10 Be surface exposure dating of erratic boulders and glacially eroded bedrock from the three areas. Our results indicate that the last BIIS covered all of northern Scotland during the LGM, but that widespread deglaciation of Caithness and Orkney occurred prior to rapid warming at ca. 14.5 ka. Copyright © 2008 John Wiley & Sons, Ltd.

Bibliographic Information

JournalJournal of Quaternary Science
PublisherWiley
Publication Date2008-02-01
Publication Year2008
Volume23
Issue2
Pages101-107
Document TypeJournal Article
Print ISSN0267-8179
eISSN1099-1417
DOI10.1002/jqs.1161
SubjectEarth & Environmental Science

Access Information

NARA Access Coverage1996-01-01~Current
Journal Homepagehttps://onlinelibrary.wiley.com/loi/10991417
Publisher PageOpen Publisher Page
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