Mancos State Park | |
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IUCN category V (protected landscape/seascape) | |
Location | Mancos, Montezuma, Colorado, United States |
Coordinates | 37°24′1″N108°16′12″W / 37.40028°N 108.27000°W Coordinates: 37°24′1″N108°16′12″W / 37.40028°N 108.27000°W |
Area | 553 acres (224 ha) |
Established | 1987 |
Governing body | Colorado Parks and Wildlife |
Mancos State Park is a Colorado state park. It is located near Mesa Verde National Park, the West Mancos Trail and the San Juan Skyway. [1] The park is known to have been a dwelling place for Ancestral Puebloans. They lived in the Four Corners area in ancient times from AD 1 to 1300. It was also later controlled by the Spanish for 200 years from the 17th to the 19th century.
In 1948 the U.S. Bureau of Reclamation commissioned the Jackson Gulch Dam, and it was officially included as a part of the Colorado state parks in 1987. [1]
Montezuma County is the southwesternmost of the 64 counties in the U.S. state of Colorado. As of the 2020 census, the population was 25,849. The county seat is Cortez.
The Town of Mancos is a Statutory Town located in Montezuma County, Colorado, United States. The town population was 1,336 at the 2010 United States Census.
The Gunnison River is located in western Colorado, and it is one of the largest tributaries of the Colorado river. The 180-mile (289-km) long river flows east to west, and it has a drainage area of 7,923 square miles (20,520 km2) according to the USGS. The drainage basin of the Gunnison River collects water from different habitats, such as forests and alpine meadows, located the along Continental Divide. As the river flows westward, it carves through the San Juan Mountains. It flows into the Colorado River at Grand Junction.
Southwestern Colorado is a region in the southwest portion of Colorado, which in turn is part of the larger Four Corners region. It is bordered by Western Colorado, Southern Colorado, the south portion of Central Colorado, Utah, and New Mexico.
The Ute Mountain Ute Tribe is one of three federally recognized tribes of the Ute Nation, and are mostly descendants of the historic Weeminuche Band who moved to the Southern Ute reservation in 1897. Their reservation is headquartered at Towaoc, Colorado on the Ute Mountain Ute Indian Reservation in southwestern Colorado, northwestern New Mexico and small sections of Utah.
There are more than 1,500 properties and historic districts in Colorado listed on the National Register of Historic Places. They are distributed over 63 of Colorado's 64 counties; only the City and County of Broomfield has none.
The West Elk Mountains are a high mountain range in the west-central part of the U.S. state of Colorado. They lie primarily within the Gunnison National Forest, and part of the range is protected as the West Elk Wilderness. The range is primarily located in Gunnison County, with small parts in eastern Delta and Montrose counties.
Crested Butte is a prominent mountain summit in the Elk Mountains range of the Rocky Mountains of North America. The 12,168-foot (3,709 m) peak is in Gunnison National Forest, 2.1 miles (3.4 km) northeast by east of the Town of Crested Butte in Gunnison County, Colorado, United States. Ski lifts and runs of the Crested Butte Mountain Resort occupy the north side of the mountain.
State Highway 184 is a 26.599 mi (42.807 km) long state highway in the southwestern corner of Colorado. SH 184's western terminus is at U.S. Route 491 near Lewis, and the eastern terminus is at U.S. Route 160 Business in Mancos.
The Pierre Shale is a geologic formation or series in the Upper Cretaceous which occurs east of the Rocky Mountains in the Great Plains, from Pembina Valley in Canada to New Mexico.
Raven Ridge is a starkly visible sedimentary rock exposure located in Rio Blanco County, Colorado and Uintah County, Utah, USA. It is managed by the Bureau of Land Management. The ridge contains a diverse selection of rare plants unique to the state of Colorado.
The Point Lookout Sandstone is a Cretaceous bedrock formation occurring in New Mexico and Colorado.
The Mancos Shale or Mancos Group is a Late Cretaceous geologic formation of the Western United States.
The Mancos River, formerly also El Rio de San Lazaro, is an 85.4-mile-long (137.4 km) northeast tributary of the San Juan River. It flows from the confluence of West Mancos River and East Mancos River near Mancos, Colorado and joins the San Juan near Four Corners Monument in New Mexico.
The Mancos High School, at 350 Grand Ave. in Mancos, Colorado, was built in 1909.
The Cliff House Sandstone is a late Campanian stratigraphic unit comprising sandstones in the western United States.
The Neo-Inca State, also known as the Neo-Inca state of Vilcabamba, was the Inca state established in 1537 at Vilcabamba by Manco Inca Yupanqui. It is considered a rump state of the Inca Empire (1438–1533), which collapsed after the Spanish conquest in the mid-1530s. The Neo-Inca State lasted until 1572, when the last Inca stronghold was conquered, and the last ruler, Túpac Amaru, was captured and executed, thus ending the political authority of the Inca state.
The Mancos Opera House, at 136 W. Grand Ave. in Mancos, Colorado, was built in 1910. It was listed on the National Register of Historic Places in 1988. It has also been known as Checkerboard Hall.
Point Lookout is an 8,427-foot elevation sandstone summit located in Mesa Verde National Park, in Montezuma County of southwest Colorado. This prominent landmark is situated 2 miles (3.2 km) south of the park entrance, and 9.3 miles (15.0 km) east-southeast of the town of Cortez, and towers 1,600 feet above the surrounding terrain of Mancos Valley. Soldiers from Fort Lewis army post used its lofty position to send heliographic signals to troops campaigning in the west. A trail climbs 2.2 miles round-trip to the top and offers views of Montezuma and Mancos valleys, as well as the La Plata Mountains. This geographical feature's name was officially adopted in 1934 by the U.S. Board on Geographic Names.