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Pre-Late Devensian high-arctic marine deposits in SW Scotland

J.D. Peacock and J.D. Everest
Scottish Journal of Geology, 46, 89-92, 10 May 2010, https://doi.org/10.1144/0036-9276/01-390
J.D. Peacock
British Geological Survey, Edinburgh EH9 2BN, UK
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J.D. Everest
British Geological Survey, Edinburgh EH9 2BN, UK
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  • For correspondence: jdev@bgs.ac.uk
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Abstract

Synopsis We present new interpretations of Digital Elevation Model (DEM) data and marine fossils collected from three sites on the Rhins of Galloway which, contrary to recent proposals, suggest that the landforms and deposits of the region do not represent evidence for a readvance during the Lateglacial Period. Rather we suggest that the high-arctic fauna found in the region are representative of an earlier, colder part of a Middle Devensian ice-free interval. The predominantly streamlined topography, and distinct lack of identifiable discrete moraine limits argues for only minor, local glacial advances, in combination with widespread rapid retreat across the peninsula at the end of the Lateglacial.

  • © 2010 Scottish Journal of Geology
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Scottish Journal of Geology: 46 (1)
Scottish Journal of Geology
Volume 46, Issue 1
May 2010
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Pre-Late Devensian high-arctic marine deposits in SW Scotland

J.D. Peacock and J.D. Everest
Scottish Journal of Geology, 46, 89-92, 10 May 2010, https://doi.org/10.1144/0036-9276/01-390
J.D. Peacock
British Geological Survey, Edinburgh EH9 2BN, UK
  • Find this author on Google Scholar
  • Find this author on PubMed
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J.D. Everest
British Geological Survey, Edinburgh EH9 2BN, UK
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
  • For correspondence: jdev@bgs.ac.uk

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Pre-Late Devensian high-arctic marine deposits in SW Scotland

J.D. Peacock and J.D. Everest
Scottish Journal of Geology, 46, 89-92, 10 May 2010, https://doi.org/10.1144/0036-9276/01-390
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