Abstract
CHARLESWORTH1 wrote that the Newer Drift glaciation of Wales reached Swansea Bay and included much of the Vale of Glamorgan (Fig. 1). Recently the line of the “South Wales End-Moraine” has been modified2 along its western fringes, and Bowen3 believes that… “The last glaciation of Gower must … be Saale”, which suggests modification of part of the southern limit of Charlesworth's line.
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References
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LEWIS, C. The Breconshire End-moraine. Nature 212, 1559–1561 (1966). https://doi.org/10.1038/2121559a0
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DOI: https://doi.org/10.1038/2121559a0
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