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The Geology and Fossils of Carriacou, West Indies

Published online by Cambridge University Press:  01 May 2009

C. T. Trechmann
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Carriacou, the largest of the Grenadines lying between Grenada and St. Vincent, is the only one, so far as is known, of that group of islands which is not predominantly volcanic in origin. It may be described as the only limestone, or largely limestone, island in the whole inner arc of the Lesser Antilles which comprises Grenada, the Grenadines, St. Lucia, Martinique, Guadeloupe (west half), Montserrat, Nevis, St. Kitts, St. Eustatius, and Saba. Carriacou is 6¾ miles long and 2⅓ in greatest width and at High North Hill and Chapeau Carré rises to 980 and 960 feet. The remainder of the island is rugged and has several lesser peaks and a central ridge, running roughly north to south, 600–830 feet in height.

Type
Original Articles
Information
Geological Magazine , Volume 72 , Issue 12 , December 1935 , pp. 529 - 555
Copyright
Copyright © Cambridge University Press 1935

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References

page 530 note 1 Geol. Mag., 1897, p. 420.Google Scholar

page 531 note 1 Quart. Journ. Geol. Soc., 1902, vol. lviii, p. 346.Google Scholar

page 531 note 2 Geol. Survey of Grenada and the (Grenada) Grenadines. Grenada Govt. Printing Office, 1924, p. 7.Google Scholar

page 534 note 1 Artesian Water Supply of Carriacou. Grenada Govt. Printing Office, 1935.Google Scholar

page 535 note 1 Woodring, Miocene Mollusks from Bowden. Publ. Carnegie Inst., 1928, p. 64.Google Scholar

page 535 note 2 Geological Survey of Grenada and the Grenada Grenadines. Grenada Govt. Printing Office, 1924, p. 3.Google Scholar

page 536 note 1 Sur l’âge des formations volcaniques anciennes de Martinique. Comptes Rend. Acad. Sci., 1902, cxxxv, pp. 1377–9.Google Scholar

page 536 note 2 L’Barrabé, . Sur l’affleurement du socle ancien des Petites Antilles dans l’île de la Desirade (Guadeloupe). Comptes Rendus des séances de l’acad. Sciences, 01 29, 1934, p. 487.Google Scholar

page 537 note 1 L.Barrabé Sur la transgression tertiaire qui a recouvert la partie orientale de la Guadeloupe. Ibid., tome 198, No. 8, 02., 1934, p. 758.

page 540 note 1 Bull. Amer. Pal., 1927, vol. 13, No. 49, p. 21, pis. 10 and 11.Google Scholar

page 540 note 2 Ibid., 1927, vol. 13, No. 49, p. 33, pl. 18, figs. 3 and 6; pl. 19, fig. 4.

page 541 note 1 Jahrb. K. K. Beichsanst., 1908, 58, p. 728, pl. xxviii, fig. 11.Google Scholar

page 542 note 1 Woodring, , Brown, , and Burbank, . “Geology of Haiti,” 1924, pl. xv, figs. 4 and 5.Google Scholar

page 542 note 2 Woodring, et al. , loc. cit., pl. xv, figs. 6, 7.Google Scholar

page 542 note 3 English, W. A., Univ. Calif. Publ., 1914, vol. 8, No. 10, p. 251, pl. 25, figs. 7 and 8.Google Scholar

page 543 note 1 Bull. Amer. Pal., 1917, vol. 29, p. 109, pl. 17, fig. 9.Google Scholar

page 543 note 2 Quart. Journ. Geol. Soc., 1849 (1850), vol. vi, p. 47, pl. x, fig. 3.Google Scholar

page 544 note 1 Quart. Journ. Geol. Soc., 1849 (1850), vol. 6, p. 46, pl. ix, fig. 5.Google Scholar

page 545 note 1 “Geology of the Republic of Haiti,” 1924, pi. xv, figs. 1, 2.Google Scholar

page 546 note 1 Bull. Amer. Pal., 1922, 39, p. 53, Pl. 3, fig. 1.Google Scholar