Coral Reef to Eolianite Transition in the Pleistocene Rocks of Great Inagua, Bahamas

Authors

Brian White, Smith College
H. Allen Curran, Smith CollegeFollow

Document Type

Conference Proceeding

Publication Date

1987

Publication Title

Proceedings of the 3rd Symposium on the Geology of the Bahamas

Abstract

Great Inagua Island, the southernmost of the chain of Bahamian islands, lies approximately 100 km northeast of the eastern tip of Cuba. This paper reports the results of reconnaissance geologic field work conducted on Great Inagua Island in January, 1985, and of more detailed observations made in January, 1986, near Matthew Town, between South West Point and Devil's Point.

First Page

165

Last Page

179

Creative Commons License

This work is licensed under a Creative Commons Attribution 4.0 International License.

Comments

Reprinted with permission from: H. Allen Curran (ed.), 1987, Proceedings of the 3rd Symposium on the Geology of the Bahamas: San Salvador, CCFL Bahamian Field Station.

Recommended Citation

White, Brian and Curran, H. Allen, "Coral Reef to Eolianite Transition in the Pleistocene Rocks of Great Inagua, Bahamas" (1987). Geosciences: Faculty Publications, Smith College, Northampton, MA.
https://scholarworks.smith.edu/geo_facpubs/99