A note on the glacial and late glacial h
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Derek Flinn
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Article
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2007
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John Wiley and Sons
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English
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## Abstract It is generally accepted that in the last glaciation Scottish ice from the Moray Firth flowed to the northwest across Caithness depositing shelly drift. Examination of striae along the east coast of Caithness shows that some were formed by ice flowing into and not out of the Moray Firth