Hostname: page-component-cd9895bd7-jkksz Total loading time: 0 Render date: 2024-12-23T20:46:36.108Z Has data issue: false hasContentIssue false

The Cretaceous and Tertiary Question in Jamaica

Published online by Cambridge University Press:  01 May 2009

Extract

The geology of Jamaica compared with that of some areas of the earth's crust is neither very involved nor very difficult of interpretation. Considering the length of time that has elapsed since it was first studied and the easy accessibility of many parts of the island, it should be fairly well known and should form a key for the interpretation of the structure of the larger and less well-known islands of Haiti and Cuba, and also of Porto Rico and the smaller islands forming the group of the Greater Antilles.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1922

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 422 note 1 Cockpit Country is the name given to an area in the north-western central part of Jamaica, but sinks of more or less cockpit-like shape are developed wherever the White Limestone forms plateaux or elevated tracts.Google Scholar

page 423 note 1 Remarks on the Geology of Jamaica”: Trans. Geol. Soc. London, 1827, vol. ii, No. 36.Google Scholar

page 423 note 2 Haug, E., Traité de Géologie II. Periodes Géologiques, p. 1525.Google Scholar

page 424 note 1 Reports on the Geology of Jamaica: Sawkins, J. G., F.G.S., and others. Appendix by R, Etheridge, F.G.S., etc., 1869, p. 307.Google Scholar

page 424 note 2 Ibid., p. 152.

page 424 note 3 The Geology and Physical Geography of Jamaica”: Bulletin of the Museum of Comparative Zoology, Harvard, vol. xxxiv, 1899, p. 82.Google Scholar

page 424 note 4 Ibid., p. 123.

page 426 note 1 Loc. cit., p. 59.Google Scholar

page 427 note 1 Loc. cit., p. 129.Google Scholar

page 429 note 1 Dr. Matley suggested to me, what I had once or twice vaguely suspected, his opinion that the Richmond beds may possibly replace the Yellow Limestone in some parts, though in some areas, such as Glasgow in the extreme north-west, both the Richmond beds and the Yellow Limestone occur. It is to be hoped that further research both in the field and also on the fossils may assist in determining this question.Google Scholar