The Windward Passage is a strait in the Caribbean Sea, between the islands of Cuba and Hispaniola. The strait specifically lies between the easternmost region of Cuba and the northwest of Haiti. 80 km (50 mi) wide, the Windward Passage has a threshold depth of 1,700 m (5,600 ft).
With Navassa Island on its southern approach, it connects the Atlantic Ocean to the Caribbean Sea, and is in the direct path of shipping between the Panama Canal and the eastern seaboard of the United States.
The Septentrional-Oriente fault zone passes through the Windward Passage from the southern coast of Cuba to the northern coast of Hispaniola. During the Holocene the slip rate between these two islands was 9 ± 3 mm (0.35 ± 0.12 in)/year. The Septentrional Fault extends east at least to the still active Mona Rift in the Mona Passage, where extension occur between Hispaniola and Puerto Rico.
- Riley, Shannon Rose (2006). Imagi-Nations in black and white: Cuba, Haiti, and the performance of difference in United States national projects, 1898-1940 (Thesis). University of California, Davis. p. 50. OCLC 191680434.[dead link]
- Lapidus, Benjamin L. "Stirring the Ajiaco: Changüí, Son, and the Haitian Connection." In Cuban Counterpoints: The Legacy of Fernando Ortiz, edited by Mauricio A. Font and Alfonso W. Quiroz, 237-45. Lanham: Lexington Books, 2005.
- Symithe, S.; Calais, E.; Chabalier, J. B.; Robertson, R.; Higgins, M. (2015). "Current block motions and strain accumulation on active faults in the Caribbean." (PDF). Journal of Geophysical Research: Solid Earth 120 (5). doi:10.1002/2014JB011779. Retrieved August 2015.
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