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dc.contributor.authorBallantyne, Colin K.
dc.contributor.authorFabel, Derek
dc.contributor.authorGheorghiu, Delia
dc.contributor.authorRodés, Ángel
dc.contributor.authorShanks, Richard
dc.contributor.authorXu, Sheng
dc.identifier.citationBallantyne , C K , Fabel , D , Gheorghiu , D , Rodés , Á , Shanks , R & Xu , S 2017 , ' Late Quaternary glaciation in the Hebrides sector of the continental shelf : cosmogenic nuclide dating of glacial events on the St Kilda archipelago ' , Boreas , vol. 46 , no. 4 , pp. 605-621 .
dc.identifier.otherPURE: 249811601
dc.identifier.otherPURE UUID: 32f8f27e-2cc9-4230-89f3-48292286c7cf
dc.identifier.otherBibtex: urn:26d95a081dd403ae48762588b038e155
dc.identifier.otherScopus: 85018789165
dc.identifier.otherWOS: 000412097800001
dc.descriptionThe authors thank NERC-CIAF for funding analysis of the 10Be and 36Cl exposure ages (Allocation 9116/0412), the Carnegie Trust for the Universities of Scotland for a grant towards travel expenses.en
dc.description.abstractThe St Kilda archipelago lies ~65 km west of the Outer Hebrides and ~60 km east of the Atlantic shelf break, and represents a key site for testing the assertion that during the Last Local Glacial Maximum (LLGM; c. 27 ka) the British–Irish Ice Sheet (BIIS) extended to near the shelf edge in all sectors. Two consistent cosmogenic 36Cl exposure ages averaging (≥) 81.6±7.8 ka for perched boulders at 290 m altitude demonstrate that the last ice sheet failed to over-run high ground on the largest island, Hirta. 36Cl and 10Be exposure ages for glacially emplaced boulders on low ground indicate deposition by small, locally nourished glaciers that last occupied a north-facing valley (Gleann Mòr) at c. 30.9±3.2 ka, prior to extension of the last ice sheet to the outer shelf, and a south-facing valley (Village Bay) at c. 19.2±2.3 ka, several millennia after the LLGM. Our dating evidence is consistent with previous interpretations of lithostratigraphical, seismostratigraphical and geomorphological evidence and confirms that the last ice sheet failed to encroach on St Kilda. A simple ice-flow model demonstrates that even if thin, low-gradient ice lobes encircled the archipelago during the LLGM, the ice margin can only have reached the outermost moraine banks, ~40 km west of St Kilda, under extremely low (<2 kPa) driving stresses, implying either surge-like transient streaming behaviour at the ice-sheet margin or that the moraine banks relate to an earlier, more extensive ice sheet. The final glaciation of the Village Bay area at c. 19.2±2.3 ka was out of phase with the behaviour of the BIIS, which was undergoing net retreat during this period.
dc.rights© 2017 Collegium Boreas. Published by John Wiley & Sons Ltd. This work has been made available online in accordance with the publisher’s policies. This is the author created accepted version manuscript following peer review and as such may differ slightly from the final published version. The final published version of this work is available at:
dc.subjectGE Environmental Sciencesen
dc.titleLate Quaternary glaciation in the Hebrides sector of the continental shelf : cosmogenic nuclide dating of glacial events on the St Kilda archipelagoen
dc.typeJournal articleen
dc.contributor.institutionUniversity of St Andrews.School of Geography and Geosciencesen
dc.contributor.institutionUniversity of St Andrews.School of Geography & Sustainable Developmenten
dc.description.statusPeer revieweden

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