Lowe, J., Matthews, I., Mayfield, R., Lincoln, P., Palmer, A., Staff, R. and Timms, R. (2019) On the timing of retreat of the Loch Lomond (‘Younger Dryas’) Readvance icefield in the SW Scottish Highlands and its wider significance. Quaternary Science Reviews, 219, pp. 171-186. There may be differences between this version and the published version. You are advised to consult the publisher’s version if you wish to cite from it. http://eprints.gla.ac.uk/192781/ Deposited on: 12 August 2019 Enlighten – Research publications by members of the University of Glasgow http://eprints.gla.ac.uk On the timing of retreat of the Loch Lomond (‘Younger Dryas’) Readvance icefield in the SW Scottish Highlands and its wider significance John Lowe 1#, Ian Matthews 1, Roseanna Mayfield 1*, Paul Lincoln 1, Adrian Palmer1, Richard Staff 2 †, Rhys Timms 1 1 Centre for Quaternary Research (CQR), Department of Geography, Royal Holloway University of London, Egham, Surrey, UK, TW20 0EX.
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[email protected] 2 Oxford Radiocarbon Accelerator Unit (ORAU), University of Oxford, Dyson Perrins Building, South Parks Road, Oxford OX1 3QY *Current address: Department of Geography, Southampton University, University Road Southampton SO17 1BJ.
[email protected] †Current address: Scottish Universities Environmental Research Centre (SUERC), University of Glasgow, Rankine Avenue, East Kilbride, UK, G75 0QF
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[email protected] Abstract It has long been assumed that the last glacier expansion in the Scottish Highlands, the Loch Lomond Readvance (LLR), resulted from a cold reversal that was broadly coeval with the ‘Younger Dryas’ episode.