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IV.—On the Correlation of the Palæozoic Rocks of South Africa

Published online by Cambridge University Press:  01 May 2009

Walcot Gibson
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Extract

The ancient rocks of Prieska are extensively developed in Griqualand West, where they build up the elevated Campbell Rand plateau and the lofty ranges of the Langebergen Mountains situated to the west of the Orange River Colony. The order of succession, which is much disguised by faulting and folding, has been described in great detail by Mr. G. W. Stow, whose descriptions render it evident that the rocks of these regions resemble the older strata which extend over such vast areas in the Transvaal.

Type
Original Articles
Information
Geological Magazine , Volume 9 , Issue 5 , May 1902 , pp. 210 - 213
Copyright
Copyright © Cambridge University Press 1902

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References

page 210 note 2 Q.J.G.S., vol. xxx (1874), pp. 581–680.Google Scholar

page 211 note 1 DrMolengraaff, G. A. F.: Bull. Soc. Géol. France, 1901, ser. iv, t. 1.Google Scholar

page 211 note 2 See also Gibson, W.: Geol. Mag., Dec. IV, Vol. IV (1897), pp. 548–550.CrossRefGoogle Scholar

page 211 note 3 Gibson, W.: Q.J.G.S., vol. xlviii (1892), pp. 404–437.CrossRefGoogle Scholar

page 212 note 1 Hatch, F. H.: Q.J.G.S., vol. liv (1898), p. 85.Google Scholar

page 212 note 2 Truscott, S. J.: “The Witwatersrand Goldtields; Banket and Mining Practice,” 1898, p. 109.Google Scholar

page 212 note 3 Hatch, F. H.: op. cit., p. 79.Google Scholar

page 212 note 4 Truscott, S. J.: op. cit., p. 13.Google Scholar