## 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
Note on simulating the size distribution of glacial cirques
β Scribed by Fabio V. De Blasio
- Publisher
- John Wiley and Sons
- Year
- 2002
- Tongue
- English
- Weight
- 67 KB
- Volume
- 27
- Category
- Article
- ISSN
- 0360-1269
- DOI
- 10.1002/esp.307
No coin nor oath required. For personal study only.
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