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The Loch Lomond Stadial in the British Isles

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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