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...

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Bibliographic Details
Published in:Scottish Journal of Geology
Main Author: Ballantyne, Colin Kerr
Format: Article in Journal/Newspaper
Language:English
Published: 1999
Subjects:
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