Loch Lomond Glaciation

Produced by the BBC for the British Open University

Examines the geophysical evidence that a massive ice sheet retreated about 12,500 years ago from Scotland and Northern England but returned about 1,500 years later. Explains how this glacial movement, known as the Loch Lomond readvance, is inferred from evidence of sediments found at various sites in its locality. From the Surface and sedimentary processes -- case studies in Earth sciences series

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