Goy Goy, José LuisCorvea, Jose LuisMartinez-GrañaZazo Cardeña, CaridadDabrio González, Cristino JoséNieto, Carlos E.Bustamante, Irene de2026-02-242026-02-242026-02-03Goy, J. L., Corvea, J. L., Martinez-Graña, A. M., Zazo, C., Dabrio, C. J., Nieto, C. E., & De Bustamante, I. (2026). Geomorphotectonic approach to geology of the viñales national park, cuba. Journal of Maps, 22(1), 2614771. https://doi.org/10.1080/17445647.2026.261477110.1080/17445647.2026.2614771https://hdl.handle.net/20.500.14352/133084The geological substratum of Viñales National Park is crossed by fractures and over-thrusts. It includes siliciclastic (Jurassic San Cayetano Formation), carbonate (Late Jurassic to Early Eocene Jagua, Guasasa, Pons and Ancón Formations) and olistostrome (Early-Middle Eocene Manacas Formation) rocks, covered by Quaternary deposits. Cartographic methodology includes Fundamental maps (geologic formations, Quaternary, tectonics and geomorphology) and Auxiliary maps (substratum-structures-drainage, slopes and lithology). Auxiliary maps provide basic information, whereas fundamental maps contribute, by means of superposition and selection, to elaborating the final geomorph-tectonic map as an essential part of the geological map. Results and conclusions are derived from the various cartographies.engAttribution-NonCommercial 4.0 Internationalhttp://creativecommons.org/licenses/by-nc/4.0/journal article1744-5647https://doi.org/10.1080/17445647.2026.2614771https://www.tandfonline.com/doi/full/10.1080/17445647.2026.2614771open access551.4Geologic formationsQuaternaryGeomorphologymorph-tectonics Viñales National ParkCubaGeodinámica2506.07 Geomorfología