Abstract
During the last very cold period in the British Isles, which occurred more than 10,000 radiocarbon years ago, glaciers developed in many mountain areas, permafrost was extensive, frost break-up of rocks was severe (its effects including a pronounced coastal platform and cliff), downslope movement of debris was greatly accelerated, many rivers spread coarse debris over low ground, the vegetation was transformed and the fauna was greatly affected.
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Sissons, J. The Loch Lomond Stadial in the British Isles. Nature 280, 199–203 (1979). https://doi.org/10.1038/280199a0
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DOI: https://doi.org/10.1038/280199a0
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