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The Igneous and Associated Ordovician Rocks of Baxter's Bank, Radnorshire

Published online by Cambridge University Press:  01 May 2009

R. O. Roberts
Affiliation:
University College of Wales, Aberystwyth.

Extract

The area described in this paper is about 5 miles east of Rhayader and 4 miles north of Llandrindod Wells. The igneous rocks come to the surface in two localities, namely Baxter's Bank and Caerfagu Mill. The former is approximately half a mile north of the main road from Rhayader to Pen-y-Bont, whilst the latter is situated immediately to the south of the main road and about three-quarters of a mile south-east of the village of Nantmel.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1927

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References

LIST OF REFERENCES

(1) SirMurchison, R. I. Silurian System, 1839, pp. 318 et seq.Google Scholar
(2) SirRamsay, A. C. and Aveline, W. T. Q.J.G.S., iv, 1848, p. 294.CrossRefGoogle Scholar
(3) Geol. Surv. of Great Britain. Sheet 56, N.W., Old Series, 1850.Google Scholar
(4) SirMurchison, R. I. Proc. Geol. Soc., ii, 1834, pp. 85 et seq.Google Scholar
(5) Pugh, W. J. Q.J.G.S., lxxix, 1923, p. 508.CrossRefGoogle Scholar
(6) Jones, O. T. Q.J.G.S., lxxxi, 1925, p. 344.CrossRefGoogle Scholar
(7) Andrew, G. Q.J.G.S., lxxxi, 1925, p. 389.CrossRefGoogle Scholar
(8) Jones, O. T. and Andrew, G. Q.J.G.S., lxxxi, 1925, p. 407.Google Scholar
(9) Stamp, L. D. and Wooldridge, S. W. Q.J.G.S., lxxix, 1923, p. 16.CrossRefGoogle Scholar
(10) Davies, K. A. Q.J.G.S., lxxxii, 1926, p. 436.CrossRefGoogle Scholar
(11) Smith, H. G. Geol. Mag., 1918, p. 500.CrossRefGoogle Scholar