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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 ...
One of the most diverse floral communities is found near Fort Wingate, New Mexico. Paleobotanists have traditionally placed the Fort Wingate plant beds into the Monitor Butte Member , though more recently they are placed within the Bluewater Creek Formation , a subunit of the Chinle Formation first defined in 1989. [ 62 ]
Los Lunas Decalogue Stone in situ in 1997. The Los Lunas Decalogue Stone is a hoax associated with a large boulder on the side of Hidden Mountain, near Los Lunas, New Mexico, about 35 miles (56 km) south of Albuquerque, that bears a nine-line inscription carved into a flat panel. [1] The stone is also known as the Los Lunas Mystery Stone or ...
The ancient sea, which existed from the early Late Cretaceous (100 Ma) to the earliest Paleocene (66 Ma), connected the Gulf of Mexico to the Arctic Ocean. The two land masses it created were Laramidia to the west and Appalachia to the east. At its largest extent, it was 2,500 feet (760 m) deep, 600 miles (970 km) wide and over 2,000 miles ...
www.nmsu.edu. New Mexico State University (NMSU or NM State) is a public land-grant research university in Las Cruces, New Mexico. 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 as ...
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.
The Padilla Mountains form the western boundary of the Malpai. Elevations of the valleys range from about 3,700 ft (1,100 m) to 5,200 ft (1,600 m). The highest mountain in the region is Animas Peak with an elevation of 8,565 ft (2,611 m). The mountain ranges are called sky islands as they rise steeply above the desert valleys. The Sky Islands ...