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