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Paleoenvironments and landscape history of the Minor Kuril Islands since the Late Glacial

✍ Scribed by Nadezhda G. Razjigaeva; Larisa A. Ganzey; Nina I. Belyanina; Tatyana A. Grebennikova; Kirill S. Ganzey


Book ID
116854212
Publisher
Elsevier Science
Year
2008
Tongue
English
Weight
722 KB
Volume
179
Category
Article
ISSN
1040-6182

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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