Basaseachic Falls National Park
| Basaseachic Falls National Park | |
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IUCN category II (national park)
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| Location | Ocampo Municipality, Chihuahua, Mexico |
| Nearest city | Ocampo, Chihuahua |
| Coordinates | 28°07′59″N 108°15′00″W / 28.13306°N 108.25000°WCoordinates: 28°07′59″N 108°15′00″W / 28.13306°N 108.25000°W |
| Area | 5,803 hectares (14,340 acres) |
| Established | February 2, 1981 |
| Governing body | Secretariat of the Environment and Natural Resources |
Basaseachic Falls National Park is a national park located in the western side of the state of Chihuahua in the heart of the Sierra Madre Occidental mountain range. The park is named after Basaseachic Falls (Cascada de Basaseachic) the second tallest waterfall in Mexico with a height of 246 meters (853 ft). Basaseachic Falls empties into Candameña Canyon (Barranca de Candameña) which was carved by the Basaseachic River over millions of years. The park is known for its pine-oak forest, rock formations, and scenic views from high cliffs. Cliffs in the park reach an impressive height of 1,640 meters (5,380 ft).
Basaseachic Falls were discovered by Europeans sometime in the 18th century, becoming one of the most popular tourist attraction of the state of Chihuahua. The area of the present day national park was inhabited by Tarahumara prior to the Spanish Colonial period. The etymology of the name "Basaseachic" originates from the Tarahumara language, Rarámuri meaning "place of the waterfall".
The first known European settlement in the area was Misión de Tomochi near the town of Cajurichi which was under the legal jurisdiction of the mission. After the 18th century the area attracted many settlers because of the discovery of abundant natural resources like minerals and high quality wood.
Basaseachic Falls National Park was created by the Mexican federal government on February 2, 1981, by decree under president Jose Lopez Portillo. The park was defined to 5,803 hectares (14,340 acres) in the Sierra Madre Occidental along the surrounding area of the Basaseachic Falls and Barranca de Candameña.
The park is located in the subdivision of the Sierra Madre Occidental known as Sierra Tarahumara, near the municipality of Ocampo, Chihuahua. The dramatic topology was created by deep tectonic plate movements causing large fractures and rising rifts. The violent movement of the terrain resulted in deep canyons and high mountains. The present day topology has been changed over thousands of years by wind erosion and the Basaseachic River.
The vertically pronounced walls of the Candameña Canyon can reach a height of 1,640 meters (5,380 ft); Candameña Canyon is known as one of the deepest canyons in the Sierra Tarahumara. The park includes two rivers: Duraznos River and Basaseachic River; both rivers feed into Basaseachic Falls that empties into the Candameña Canyon finally ending in the Candameña River.
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Wikipedia