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III.—Axinite Veins in the Penmaenmawr Porphyrite

Published online by Cambridge University Press:  01 May 2009

Extract

In the course of a visit to North Wales last summer my friend Mr. Ivor E. Davies, of Penmaenmawr, called my attention to a mauve mineral, forming thin veins, in the intrusive porphyrite of Penmaenmawr Mountain. The specimens containing the veins were not seen in place, but were collected from the waste-heaps of the Graig Lwyd Quarries, the most easterly of the large quarries that are making such deadly inroads into the heart of the mountain. Careful search on the waste-heaps enabled us to collect further specimens, and in some of these the mineral had built in fissures and cracks somewhat crowded, very sharp-edged crystals of tabular development.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1916

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References

page 6 note 1 See, for instance, Waller, , Midland Naturalist, 1885, p. 5;Google ScholarTeall, , British Petrography, 1888, p. 275;Google ScholarSchaub, , Neues Jahrbuch für Mineralogie, etc., Abh., pp. 108 et seq., 1905;Google Scholar, Geol. Mag., Dec. VI, Vol. II, pp. 20–1, 1915.Google Scholar

page 6 note 2 Petrographic Methods, trans. Clark, , 1912, p. 366.Google Scholar

page 6 note 3 Weinschenk, op. cit., p. 367.Google Scholar

page 6 note 4 On the occurrence of Metamorphic Minerals in Calcareous Rocks in the Bodmin and Camelford areas, Cornwall”: Mineralogical Magazine, vol. xv, pp. 113–23, 1908.Google Scholar

page 7 note 1 Neues Jahrbuch für Mineralogie, Abh., p. 110.Google Scholar

page 7 note 2 The Geology of the Country around Bodmin and St. Austell (Mem. Geol. Surv.), 1909, p. 53.Google Scholar