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The location of the state of New Mexico. Paleontology in New Mexico refers to paleontological research occurring within or conducted by people from the U.S. state of New Mexico. The fossil record of New Mexico is exceptionally complete and spans almost the entire stratigraphic column. [1] More than 3,300 different kinds of fossil organisms have ...
Petroglyph National Monument. Petroglyph National Monument stretches 17 miles (27 km) along Albuquerque, New Mexico 's West Mesa, a volcanic basalt escarpment that dominates the city's western horizon. Authorized June 27, 1990, the 7,236 acres (2,928 ha) monument is cooperatively managed by the National Park Service and the City of Albuquerque.
Folsom site or Wild Horse Arroyo, designated by the Smithsonian trinomial 29CX1, is a major archaeological site about 8 miles (13 km) west of Folsom, New Mexico. It is the type site for the Folsom tradition, a Paleo-Indian cultural sequence dating to between 11000 BC and 10000 BC. The Folsom site was excavated in 1926 and found to have been a ...
The geology of New Mexico includes bedrock exposures of four physiographic provinces, with ages ranging from almost 1800 million years (Ma) to nearly the present day. Here the Great Plains, southern Rocky Mountains, Colorado Plateau, and Basin and Range Provinces meet, giving the state great geologic diversity.
November 16, 1907. Designated NMSRCP. May 21, 1971. Gila Cliff Dwellings National Monument is a U.S. National Monument created to protect Mogollon cliff dwellings in the Gila Wilderness on the headwaters of the Gila River in southwest New Mexico. The 533-acre (2.16 km 2) national monument was established by President Theodore Roosevelt through ...
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Mount Taylor (Navajo: Tsoodził, Navajo pronunciation: [tsʰòːtsɪ̀ɬ] means "The Great Mountain" [3]) is a dormant stratovolcano in northwest New Mexico, northeast of the town of Grants. [4] It is the high point of the San Mateo Mountains [a] and the highest point in the Cibola National Forest. It was renamed in 1849 for then- president ...
The Puye Cliff Dwellings are the ruins of an abandoned pueblo, located in Santa Clara Canyon on Santa Clara Pueblo Reservation land near Española, New Mexico.Established in the late 1200s or early 1300s and abandoned by about 1600, this is among the largest of the prehistoric Indian settlements on the Pajarito Plateau, showing a variety of architectural forms and building techniques.