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III.—The Geology of Barbados

Published online by Cambridge University Press:  01 May 2009

J. B. Harrison and
A. J. Jukes-Browne
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Extract

The August number of the Quaterly Journal of the Geological Society contains a paper on this subject by Dr. J. W. Spencer, who believes that the rocks which were described by us under the head of ‘Raised Coral Reefs’ do not form one continuous succession of Pleistocene reef-rocks, but consist of several different limestone formations. He thinks that there are three such formations, and that each is separated from the other by a break or unconformity.

Information

Type
Original Articles
Information
Geological Magazine , Volume 9 , Issue 12 , December 1902, pp. 550 - 554
Copyright
Copyright © Cambridge University Press 1902

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References

page 550 note 2 Quart. Journ. Geol. Soc., 1891, vol. xlvii, p. 209.Google Scholar

page 551 note 1 Quart. Journ. Geol. Soc, 1895, vol. li, p. 255.

page 552 note 1 A coral-reef is a composite mass of rock, and portions of it are often differently made up and are more fossiliferous than other parts of the same reef.

page 553 note 1 See Messrs. Franks & Harrison, “On the Globigerina Marls of Barbados,” in. Quart. Journ. Geol. Soc, vol. liv, p. 540.