
Cabo Corrientes is a cape on the Guanahacabibes Peninsula in Pinar del Río Province, in the west of Cuba. It is covered by a protected nature reserve. The cape has been the scene of various pirate encounters and shipwrecks. During World War II (1939–45) several ships were sunk near the cape. There is a hotel for researchers and ecotourists or scuba divers.

Cape San Antonio, is a cape which forms the western extremity of the Guanahacabibes Peninsula and the western extremity of Cuba. It extends into the Yucatán Channel, and is part of the municipality of Sandino, in Pinar del Río Province. According to the International Hydrographic Organization, it marks the division point between the Caribbean Sea to the south and Gulf of Mexico to the north.

Cayo Levisa is a cay in Pinar del Río Province, Cuba. Accessible only through boats from Palma Rubia, the white sand beaches on its north coast attract tourism. It has several snorkeling and diving sites. It is part of the Colorados Archipelago coral reef and well known for its black coral.

The Colorados Archipelago is a chain of isles and cays on Cuba's north-western coast.

The Cuban underwater formation refers to a site thought by some to be a submerged granite structural complex off the coast of the Guanahacabibes Peninsula in the Pinar del Río Province of Cuba.

The Artemisa Formation is a geologic formation in western Cuba. It preserves mainly ammonite fossils dating back to the Late Oxfordian to Tithonian period. The formation is divided into two members; La Zarza and Sumidero Members. Most of the formation was deposited in deeper marine conditions.

The Guasasa Formation is a geologic formation in Cuba. It is Tithonian to Early Valanginian in age and contains fossils of ammonites.

The Habana Formation is a geologic formation in Cuba. It preserves mainly gastropod and rudist fossils dating back to the Late Campanian to Maastrichtian periods. The formation was defined by Robert H. Palmer in 1934.

The Jagua Formation is a Late Jurassic geologic formation in the Sierra de los Órganos and Sierra del Rosario mountain ranges in Pinar del Río Province, western Cuba. Plesiosaur, pliosaur, pterosaur, metriorhynchid, turtle and dinosaur remains are among the fossils that have been recovered from its strata.

The San Cayetano Formation is a geologic formation in western Cuba. It preserves fossils of mainly ammonites dating back to the Jurassic period.

Guanahacabibes Peninsula is the westernmost point on the island of Cuba. It is located in Pinar del Río Province, in the municipality of Sandino and is sparsely populated. The waters surrounding the peninsula are important spiny lobster and red snapper fishing grounds. It also boasts the category of Biosphere Reserve, listed by UNESCO in 1987. Its western extremity, Cape San Antonio, is the westernmost point of Cuba.

Guaniguanico, also known as Cordillera de Guaniguanico, is a mountain range of western Cuba that spans from the centre-west of Pinar del Río Province to the western area of Artemisa Province. It is formed by the subranges of Sierra del Rosario and Sierra de los Órganos.

The Jabaco Formation is a geologic formation in Cuba. It preserves fossils dating back to the Paleogene period.

Sierra de los Órganos is a mountain range in the province of Pinar del Río, western Cuba. Along with the Sierra del Rosario, it is part of the Guaniguanico mountain range.

Sierra del Rosario is a mountain range in the provinces of Pinar del Río and Artemisa, western Cuba. It is located in the eastern part of the Guaniguanico range and, along with the Sierra de los Órganos, is part of it.

Viñales Valley is a karstic depression in Cuba. The valley has an area of 132 km2 (51 sq mi) and is located in the Sierra de los Órganos mountains, just north of Viñales in the Pinar del Río Province.