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The Late Pleistocene cataclysmic releases of glacial meltwater left distinct footprint across the Central European Lowland. Deeply incised tunnel valleys, oversized ice-marginal spillways, fields of mega-dunes, and glacial curvilineations carved by rapid drainage events occur along the southern margin of the last (Weichselian) Scandinavian Ice Sheet margin. These meltwater releases contributed sigThe Late Pleistocene cataclysmic releases of glacial meltwater left distinct footprint across the Central European Lowland. Deeply incised tunnel valleys, oversized ice-marginal spillways, fields of mega-dunes, and glacial curvilineations carved by rapid drainage events occur along the southern margin of the last (Weichselian) Scandinavian Ice Sheet margin. These meltwater releases contributed sig
