Pattern and timing of retreat of the last British-Irish Ice Sheet

• Published in: Quaternary Science Reviews
• Main Authors: Clark, C.D., Hughes, A.L., Greenwood, S.L., Jordan, C., Sejrup, H.P.
• Other Authors: Clark, CD
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2012
• Subjects: Ice Sheet
• Online Access: https://eprints.whiterose.ac.uk/83510/; https://eprints.whiterose.ac.uk/83510/2/Pattern%20and%20timing%20of%20retreat%20of%20the%20last%20British-Irish%20Ice%20Sheet%20-%20Figures.pdf; https://eprints.whiterose.ac.uk/83510/8/Pattern%20and%20timing%20of%20retreat%20of%20the%20last%20British-Irish%20Ice%20Sheet%20-%20QSR.pdf; https://doi.org/10.1016/j.quascirev.2010.07.019

During the last glacial the ice sheet that subsumed most of Britain, Ireland and the North Sea attained its maximum extent by 27 ka BP and with an ice volume sufficient to raise global sea level by ca. 2.5 m when it melted. We reconstruct the demise of this British-Irish Ice Sheet (BIIS) and present palaeoglaciological maps of retreat stages between 27 – 15 ka BP. The whole land area was investigated using remote sensing data and we present maps of moraines, meltwater channels, eskers, and drumlins and a methodology of how to interpret and bring them together. For the continental shelf, numerous large moraines were discovered recording an extensive pattern of retreat stretching from SW Ireland to the Shetland Isles. From an integration of this new mapping of glacial geomorphology (> 26,000 landforms) with previously published evidence, compiled in the BRITICE database, we derive a pattern of retreat for the whole BIIS. We review and compile relevant dates (881 examples) that constrain the timing of retreat. All data are held within a Geographic Information System (GIS), and are deciphered to produce a best-estimate of the combined pattern and timing of retreat.