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Published online by Cambridge University Press: 01 May 2009
Having shown that the ‘railway-cutting’ valleys of the Goathland area exhibit anomalies of position seemingly irreconcilable with the view supported by Professor Bonney that they are vestiges of an ancient river-system that has undergone readjustments by the process of stream capture, I may now enforce the argument by exhibiting the contrast between the form and magnitude of the old and those of the new valleys in the same district.
1 (1) Kendall, & Bailey, , Trans. Edin. Roy. Soc., vol. xlvi, pt. i, No. 1, 1908Google Scholar; (2) Kendall, & Muff, , Trans. Edin. Geol. Soc., vol. viii, 1903Google Scholar; (3) Smythe, , Trans. Nat. Hist. Soc. Northumberland and Durham, n.s., vol. iii, pt. i, 1908;Google Scholar(4) Dwerryhouse, , Q.J.G.S., vol. lviii, p. 572, 1902CrossRefGoogle Scholar; (5) Kendall, , Naturalist, 1912Google Scholar; (6) Jowett, & Muff, , Proc. Yorks. Geol. Soc., vol. xv, p. 193, 1904CrossRefGoogle Scholar; (7) Kendall, , Brit. Assoc. Rep., 1896Google Scholar; (8) Carter, , Proc. Yorks. Geol. Soc., vol. xv, p. 411, 1905CrossRefGoogle Scholar; (9) Kendall, ibid., p. 493; (10) Kendall, and Carter, , Proc. Geol. Assoc., vol. xix, p. 114Google Scholar; (11) Smith, , Q.J.G.S., vol. lxviii, p. 402, 1912CrossRefGoogle Scholar; (12) Jowett, , Q.J.G.S., vol. lxx, p. 199, 1915.Google Scholar