After the ice:Lateglacial and Holocene landforms and landscape evolution in Scotland
During Lateglacial cold periods, permafrost developed throughout Scotland, sediment-mantled slopes were extensively modified by solifluction and other forms of periglacial mass movement, large-scale sorted patterned ground formed on plateaux, and enhanced rockfall resulted in talus accumulation belo...
| Published in: | Earth and Environmental Science Transactions of the Royal Society of Edinburgh |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
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2019
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| Online Access: | https://research-portal.st-andrews.ac.uk/en/publications/85256fc9-0f55-4ba4-a346-707ce46bf1cb https://doi.org/10.1017/S175569101800004X https://research-repository.st-andrews.ac.uk/bitstream/10023/16465/1/Ballantyne_2018_EESTRSE_Aftertheice_AAM.pdf |