Cuban tectonics refers to the geological processes and structures that shape the island of Cuba. The region is influenced by the interaction of several tectonic plates, primarily the North American Plate, the Caribbean Plate, and the Gulf of Mexico Plate. These interactions can lead to earthquakes and the formation of mountain ranges, such as the Sierra Maestra. The tectonic activity in Cuba is characterized by both compressional and extensional forces. This results in a complex landscape, including fault lines and uplifted areas. Understanding these tectonic processes is crucial for assessing geological hazards and managing natural resources in the region.