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VI.—On the Geology of the District from Cil-y-Coed to the St. Annes–Llanllyfni Ridge (Carnarvonshire).5
Published online by Cambridge University Press: 01 May 2009
Extract
B. Pre–Cambrian, Rhyolitic Series.—(i) At the south–west end of the Craig–y–Dinas mass we find exposed a rock similar in every respect macroscopically to that which is found at Cil–y–Coed. Unfortunately it cannot be followed far, as the land is completely under drift, the top of Craig–y–Dinas itself being capped by a thick layer of drift.
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References
1 Priem, F., “Sur des Poissons et autres Fossiles du Silurien supérieur du Portugal”: Communic. Serv. Géol. Portugal, vol. viii, p. 3, pl. i, figs. 7–10, 1910.Google Scholar
2 Woodward, A. S., Catalogue of Fossil Fishes in the British Museum, pt. ii, 1891, p. 20Google Scholar. Dean, B., “Notes on Acanthodian Sharks”: Amer. Journ. Anat., vol. vii, p. 209, figs. 1–10, 1907CrossRefGoogle Scholar. Goodrich, E. S., in Lankester's Treatise on Zoology, pt. ix, 1909, p. 190, fig. 160.Google Scholar
3 Woodward, A. S., Presidential Address, Quart. Journ. Geol. Soc., vol. lxxi, p. lxvi, 1915.Google Scholar
4 Campylodus sigmoides, Rohon, J. V., loc. cit., p. 52, pl. i, fig. 25, 1893Google Scholar; C. (?) delgadoi, Priem, F., loc. cit., p. 5, pl. i, figs. 11–15, 1910.Google Scholar
1 Mem. Geol. Surv., vol. ii, p. 143, 1866.Google Scholar
1 Q.J.G.S., vol. xxxv, p. 312, 1879.Google Scholar