Skip to main content

Cuba

  • Reference work entry
World Regional Geology

Part of the book series: Encyclopedia of Earth Science ((EESS))

The island of Cuba is the largest of the Antilles, or Caribbean islands, with an area of approximately 110,922 km2 (44,218 sq mi). Its official name is “República de Cuba.” The capital is Habana (Havana) and the chief cities include Santiago de Cuba, Camagüey, Guantánamo, and Santa Clara. The island is separated from U.S. territory on the NW by a 160-km (90-mile) channel, the Straits of Florida. A large shallow intermediate bank (Cay Sal) belongs to the Bahamas. The separating Nicholas Channel is 1500 m deep. The much narrower Old Bahama Channel (600 m deep) separates Cuba on the NE from the Great Bahama Bank. To the E it is separated by the 3000-m-deep Windward Channel from Hispaniola (Haiti). On the W the Yucatan Channel and the main course of the Gulf Stream separates it from Mexico.

The main island of Cuba is 1290 km long (E-W) and 70–200 km across. There are numerous smaller offshore islands; these are mainly coral or sandcays (e.g., on the northern coast the Archipelago de...

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 519.00
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

References

  • Acevedo-Gonzales, M. J., 1967. “Classificación general y descriptción del Carso Cubana,” Inst. Nacl. Hydr., Publ. Esp. 4, 33–64.

    Google Scholar 

  • Bermudez, P. J., 1950. “Contribution al estudio del Cenozoico cubano,” Mem. Soc. Cubana Hist. Nat., 19, 205–375.

    Google Scholar 

  • Butterlin, J., 1956. La Constitution Géologique et la Structure des Antilles. Paris: Centre Nat. Rech. Sci., 453p.

    Google Scholar 

  • Corral, J. I., 1939. “La union de Cuba con el continente Americano,” Soc. cubana ing. Rev., 33(7), 581–681.

    Google Scholar 

  • Daetwyler, C. C., and Kidwell, A. L., 1959. “The Gulf of Batobano, a modern carbonate basin,” Proc. 5th World Petroleum Congr., New York, 1, 1–21.

    Google Scholar 

  • Darton, N. H., 1926. “Geology of the Guantanamo Basin, Cuba,” Wash. Acad. Sci. J., 16, 324–333.

    Google Scholar 

  • Ducloz, C., and Vuagnat, M., 1962. “A propos de place des serpentinites de Cuba,” Genève Arch. Sci., 15, 309–332.

    Google Scholar 

  • Furrazola-Bermudez, G., et al., 1964. “La Habana,” in Geológia de Cuba, vol. 1. Ed. Consejo Nac. Univer., 239p.

    Google Scholar 

  • Hatten, C. W., and Meyerhoff, A.A., 1970. “The Caribbean area: a case of destruction and regeneration of a continent, discussion,” Bull. Geol. Soc. Am., 81, 1855–1862.

    Google Scholar 

  • Itturalde-Vinent, M. A., 1972. “Principal characteristics of Oligocene and lower Miocene stratigraphy of Cuba,” Bull. Am. Assoc. Petrol. Geologists, 56(12), 2369–2379.

    Google Scholar 

  • Khudoley, K. M., 1967. “Principal features of Cuban geology,” Bull. Am. Assoc. Petrol. Geologists, 51(5), 668–677.

    Google Scholar 

  • Khudoley, K. M., and Meyerhoff, A. A., 1971. “Paleogeography and geological history of Greater Antilles,” Geol. Soc. Am. Mem. 129, 199p.

    Google Scholar 

  • Kozary, M., 1954. “Conglomerates associated with the Cubitas Plateau, Cuba,” Ph.D. thesis, Columbia Univ., 168p.

    Google Scholar 

  • Kozary, M., 1956. “Ultramafics in the thrust zones in northwestern Oriente, Cuba,” 20th Intern. Geol. Cong., Resumenes, 138–139.

    Google Scholar 

  • Kozary, M., 1968. “Ultramafic rocks in thrust zones of northwestern Oriente province Cuba,” Bull. Am. Assoc. Petrol. Geologists, 52(12), 2298–2317.

    Google Scholar 

  • Kuhlmann, D. H. H., 1970. “Die Korallenriffe Kubas. 1. Genese und Evolution,” Intern. Rev. Hydrobiol., 55(5), 729–756.

    Google Scholar 

  • Lehmann, H., Krommelbein, K., and Lotschert, W., 1956. “Karstmorphologische, geologische und botanische Studien in der Sierra de los Organos auf Cuba,” Erdkunde, 10(3), 185–203.

    Google Scholar 

  • Lewis, J. W., 1932. “Geology of Cuba,” Bull. Am. Assoc. Petrol. Geologists, 16(6), 533–555.

    Google Scholar 

  • MacGillavry, H. J., 1970. “Geological history of the Caribbean,” Proc. Kon. Ned. Akad. Wetensch. (Amsterdam), Ser. B, 73(1), 64–96.

    Google Scholar 

  • Meyerhoff, H. A., 1938. “Texture of karst topography in Cuba and Puerto Rico,” J. Geomorphol., 1, 279–295.

    Google Scholar 

  • Meyerhoff, H. A., and Hatten, C. W., 1968. “Diapiric structures in central Cuba,” in J. Braustein and G.D. Brien, eds., Diapirism and Diapirs (Mem. 8). Tulsa: Am. Assoc. Petrol. Geologists, 315–357.

    Google Scholar 

  • Meyerhoff, H. A., et al., 1969. “Geologic significance of radiometric dates from Cuba,” Bull. Am. Assoc. Petrol. Geologists, 53(12), 2494–2500.

    Google Scholar 

  • Mitchell, R. C., 1955. “The ages of the serpentinized peridotites of the West Indies,” Proc. Kon. Ned. Akad. Wetensch. (Amsterdam), Sr. B, 3, 194–212. 194–212.

    Google Scholar 

  • Nũnez-Jimenez, A., et al., eds., 1962. Mapa Geológico de Cuba. La Habana: Minist. Indust., Inst. Cub. Rec. Min., 1:1,000,000.

    Google Scholar 

  • Palmer, R. H., 1945. “Outline of the geology of Cuba,” J. Geol., 53(1),–34.

    Google Scholar 

  • Rigassi-Studer, D., 1961. “Quelques vues nouvelles sur la géologie cubaine,” Chron. Mines et Rech. Minière, 29, 3–7.

    Google Scholar 

  • Rutten, L., 1940. “On the age of the serpentines in Cuba,” Proc. Ned. Akad. Wetensch. (Amsterdam), 43, 542–547.

    Google Scholar 

  • Škvor, V., 1969. “The Caribbean area: a case of destruction and regeneration of a continent,” Bull. Geol. Soc. Am., 80(6), 961–968 (with discussion by Hatten, C. W., and Meyerhoff, A. A., 1970, Ibid., 81, 1855–1862).

    Google Scholar 

  • Taber, S., 1931. “Structure of Sierra Maestra, Cuba,” J. Geol., 39, 532–557.

    Google Scholar 

  • Taber, S., 1934. “Sierra Maestra of Cuba, part of the northern rim of the Bartlett Trough,” Bull. Geol. Soc. Am., 45, 567–620.

    Google Scholar 

Cross-references

Download references

Authors

Rights and permissions

Reprints and permissions

Copyright information

© 1975 Dowden, Hutchinson & Ross, Inc.

About this entry

Cite this entry

Fairbridge, R.W. (1975). Cuba . In: World Regional Geology. Encyclopedia of Earth Science. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-31081-1_40

Download citation

  • DOI: https://doi.org/10.1007/3-540-31081-1_40

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-0-4702-5145-4

  • Online ISBN: 978-3-540-31081-5

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics