Cuba is located in an area with several active fault systems which produce on average about 2000 seismic events each year.[1] While most registered seismic events pass unnoticed, the island has been struck by a number of destructive earthquakes over the past four centuries, including several major quakes with a magnitude of 7.0 or above.
Approximately 70% of seismic activity in Cuba emanates from the Oriente fault zone, located in the Bartlett-Cayman fault system which runs along the south-eastern coast of Cuba and marks the tectonic boundary between the North American plate and the Caribbean plate.[2] The 12 currently active faults in Cuba also include the Cauto-Nipe, Cochinos and Nortecubana faults.[2]
Destructive earthquakes originating from the Oriente fault occurred in 1766 (MI= 7.6), 1852 (MI = 7.2) and 1932 (Ms = 6.75).[3] Some studies suggested there is a high probability the Oriente fault would produce a magnitude 7 earthquake,[4] this happening in January 2020, with a magnitude of 7.7, the highest registered in this country's history.
Intensity estimated at IX EMS-98,[1] with 26 heavy aftershocks. Caused severe damage to churches and other buildings in Santiago de Cuba, as well as landslides in the Sierra Maestra region. Shaking felt in the whole of eastern Cuba, up to the islands of Jamaica and Hispaniola.[13]
A series of severe shock waves originating from western Cuba were also felt in the town of Key West (Florida), and included a strong earthquake on 23 January 1880 in San Cristóbal, Pinar del Río at 4 a.m.[16]
Intensity estimated at VIII EMS-98.[1] 8[17] – 1500[18] deaths, 300 injured. 80% of buildings in Santiago de Cuba affected.,[17] with damage totaling 15 million Pesos.[13]
Alvarez, Leonardo; Giuliano F. Panza; Franco Vaccari; Bertha E. Gonzalez (December 1999), "Modelling of seismic ground motion in Santiago de Cuba city from earthquakes in Oriente fault seismic zone", Pure and Applied Geophysics, 158 (9–10), Trieste/Miramare: The Abdus Salara International Centre for Theoretical Physics: 1763, Bibcode:2001PApGe.158.1763A, doi:10.1007/PL00001242, S2CID129225540
Calais, E.; J. Perrot; B. Mercier de Lépinay (1997). "Tectonic and Kinematic Regime along the Northern Caribbean Plate Boundary: New Insights from Broad-band Modeling of the May 25, 1992, Ms = 6.9 Cabo Cruz, Cuba, Earthquake". Pure and Applied Geophysics. 149 (3): 475–487. Bibcode:1997PApGe.149..475P. doi:10.1007/s000240050036. S2CID55729435.
Cotilla Rodriguez, M.O.; Franzke, H.J.; Córdoba Barba, D. (June 2007). "Seismicity and seismoactive faults of Cuba". Russian Geology and Geophysics. 48 (6): 505–522. Bibcode:2007RuGG...48..505C. doi:10.1016/j.rgg.2006.08.004.
Lander, James F. (1997). "Caribbean Tsunamis: An initial history"(PDF). In Ahmad, Rafi (ed.). Natural hazards and hazard management in the Greater Caribbean and Latin America. Vol. 3. Kingston: Unit for Disaster Studies, University of the West Indies. pp. 1–18. ISBN978-976-41-0115-4.
Oficina Nacional de Estadísticas (ONE) (2006). "4. Desastres naturales"(PDF). Compendio de Estadísticas del Medio Ambiente de Cuba, 1990–2004. Havana: Oficina Nacional de Estadísticas.
Oficina Nacional de Estadísticas (ONE) (2009). "Terremotos fuertes reportados en Cuba"(PDF). Anuario Estadístico de Cuba 2008. Havana: Oficina Nacional de Estadísticas.
Rubio, M. (1985). The assessment of seismic hazard for the Republic of Cuba. Prague: Ph.D. Thesis, Institute of Geophysics, Science Academy of Czechoslovakia.