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I.—The Geological History of South Africa1

Published online by Cambridge University Press:  01 May 2009

F. H. Hatch
F. H. Hatch
Affiliation:
President of the Geological Society of South Africa
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Extract

The subject of this address is a brief acount of the succession, thickness, and geological history of the South African, and more especially of the Transvaal, formations. The information necessary for such an account is of course very incomplete, but in broad outline the succession is now known, and some speculation as to the physical conditions that prevailed during the building up of the region may perhaps be permitted. I propose to deal with the period of the geological history of this country that came to an end with the close of Karroo times. The Karroo period ends with the Stormberg rocks (Rhæitic), and since that time South Africa has, with the exception of a small coastal area, been a land surface, and the rocks have consequently been exposed uninterruptedly to the forces of denudation.

Type
Original Articles
Information
Geological Magazine , Volume 3 , Issue 3 , March 1906 , pp. 97 - 104
Copyright
Copyright © Cambridge University Press 1906

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Footnotes

1

Presidential Address delivered by Dr. F. H. Hath to the Geological Society of South Africa, 29th January, 1906.

References

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page 103 note 4 Quite recently some lamellibranch remains have been found by the Cape Survey in the Table Mountain Sandstone, but have not yet been determined.

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