Maximum altitude of Late Devensian glaciation on the Isle of Mull and Isle of Jura
Evidence provided by striae, ice-moulded rock, erratics and perched boulders indicates that the last (Late Devensian) ice-sheet reached an altitude exceeding 760 m on Mull and 660 m on Jura. The highest summits on both islands support periglacial blockfields, suggesting that they remained as nunatak...
Published in: | Scottish Journal of Geology |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1999
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Online Access: | https://research-portal.st-andrews.ac.uk/en/researchoutput/maximum-altitude-of-late-devensian-glaciation-on-the-isle-of-mull-and-isle-of-jura(7fb9a68f-86f1-4cd3-b72a-d0eb266d15f4).html https://doi.org/10.1144/sjg35020097 http://www.scopus.com/inward/record.url?scp=0033380978&partnerID=8YFLogxK |