After the ice: Lateglacial and Holocene landforms and landscape evolution in Scotland
ABSTRACT 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 accumula...
| Published in: | Earth and Environmental Science Transactions of the Royal Society of Edinburgh |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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Cambridge University Press (CUP)
2018
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| Online Access: | http://dx.doi.org/10.1017/s175569101800004x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S175569101800004X |