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The “Dimlington” in the context of ice sheets refers to the Dimlington Stadial, a term used to describe the main glacial episode of the Late Devensian in Britain. This period, which lasted between 26,000 and 13,000 years before present, is characterized by the expansion of the British-Irish Ice Sheet. The Dimlington Stadial is a specific stage within the broader Late Devensian period of glaciation.
