Published online by Cambridge University Press: 29 November 2011
The fact that the Pleistocene ice-sheets mantled so great a part of Britain was long regarded as sufficient explanation of the absence of Lower Palaeolithic remains from the territory south of a line drawn from the Wash to the Bristol Channel. Recent work and finds, however, show that during genial conditions early man certainly moved quite far into areas freed by the waning ice during periods of retreat. Thus, from extremes beyond those cited, there are reports of a few Lower Palaeolithic implements from Pleistocene gravels in the valley of the Trent in Lincolnshire, from the valley of the Don and from Huntow, in Yorkshire, and of an odd piece from Cheshire. But of most import to the present study are the Lower Palaeolithic stone tools from the basin of the Severn in the Midlands, and an Acheulian hand-axe has been found within the past few months at Pen-y-lan, near Cardiff. With the palaeoliths discovered at intermediate sites in the basin of this great river the range in the Atlantic drainage is extended from Somerset into once glaciated territory.
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page 14 note 6 Ibid., pp. 530-8.
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page 21 note 1 Whereas the Riss or third glaciation comprised the greatest advance of the ice on the Continent, it was the earlier Great Eastern, Main Glaciation, or Second Great Welsh Glaciation which, with its concomitants, was the correlative of the continental Mindel or second glaciation and reached farthest in south Britain. It is particularly interesting that in England deposits as far from its main southern limits as Cornwall and Devon register the influence exerted by this powerful complex (Arkell, W. J., ‘The Pleistocene Rocks at Trebetherick Point, North Cornwall: Their Interpretation and Correlation’, in Proc. Geol. Assoc, vol. liv, 1943Google Scholar; cf. Pickard's, Colonel Ransom Presidential Address, Transactions of the Devonshire Association for the Advancement of Science, Literature and Art, 1946, vol. lxxviii, pp. 207–28)Google Scholar.
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page 22 note 3 Idem.
page 22 note 4 Wooldridge, S. W., ‘The Glaciation of the London Basin and the Evolution of the Lower Thames Drainage System’, in Quart. Journ. Geol. Soc, vol. xciv, 1938, pp. 627–67CrossRefGoogle Scholar.
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page 23 note 1 Idem in op. cit., 1945, p. 17.
page 23 note 2 Op. cit., pp. 208 and 212, and fig. 4, no. I.
page 23 note 3 Breuil and Koslowski, opp.citt., 1931 and 1932, passim.