Deglaciation chronology of the Galloway Hills Ice Centre, southwest Scotland
During the last glacial maximum, the Galloway Hills in southwest Scotland acted as a major centre of ice dispersion within the last British–Irish Ice Sheet (BIIS). Six new or recalibrated 10Be exposure ages for samples obtained from boulders near the former ice divide yielded uncertainty-weighted me...
Published in: | Journal of Quaternary Science |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Wiley
2013
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Subjects: | |
Online Access: | http://eprints.gla.ac.uk/79838/ |