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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 ...
The Hartley Mammoth Site is a pre-Clovis archaeological and paleontological site in New Mexico.Preserving the butchered remains of two Columbian mammoths, small mammals and fish, the site is notable due to its age (~37,500 BP), which is significantly older than the currently accepted dates for the settlement of the Americas.
Three Rivers Petroglyph Site. There are over 21,000 petroglyphs at the Three Rivers Petroglyph Site at Three Rivers, New Mexico, [1] located midway between Tularosa and Carrizozo in Otero County on Highway 54. Many of the petroglyphs can be easily viewed from a trail open to the public which winds through the rocks for about one mile.
Slope rating. 129. The New Mexico State University Golf Course is an 18–hole golf course within the campus of New Mexico State University, in the city of Las Cruces, New Mexico. The golf course was established in 1963 and is opened to the public. It features 4 sets of tees for different skill levels and measures 7078 yards from the longest ...
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 ...
New Mexico State University (NMSU or NM State) is a public land-grant research university in Las Cruces, New Mexico, United States. Founded in 1888, it is the state's oldest public institution of higher education, and the state's first land-grant institution in New Mexico. NMSU has campuses in Alamogordo, Doña Ana County, and Grants, as well ...
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The geologic history of the state began with its assembly during the Yavapai and Mazatzal orogenies 1750 to 1650 million years ago (Mya). This was followed by 200 million years of tectonic quiescence that ended in the Picuris orogeny. This event transformed the New Mexico crust into mature continental crust.