Hostname: page-component-848d4c4894-wg55d Total loading time: 0 Render date: 2024-06-09T14:48:44.269Z Has data issue: false hasContentIssue false

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

Published online by Cambridge University Press:  01 May 2009

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
Copyright
Copyright © Cambridge University Press 1902

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 210 note 2 Q.J.G.S., vol. xxx (1874), pp. 581680.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. 548550.CrossRefGoogle Scholar

page 211 note 3 Gibson, W.: Q.J.G.S., vol. xlviii (1892), pp. 404437.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