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The New Mexico State Capitol is the seat of government of the U.S. state of New Mexico, located in its capital city of Santa Fe. It houses both chambers of the New Mexico Legislature and the offices of the Governor, Lieutenant Governor, and Secretary of State. The building is one of only eleven state capitols without a dome, and the only ...
Folsom site. 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 ...
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 history of New Mexico is based on archaeological evidence, attesting to the varying cultures of humans occupying the area of New Mexico since approximately 9200 BCE, and written records. The earliest peoples had migrated from northern areas of North America after leaving Siberia via the Bering Land Bridge.
Santa Fe (/ ˌ s æ n t ə ˈ f eɪ, ˈ s æ n t ə f eɪ / SAN-tə FAY, - fay; Spanish:) is the capital of the U.S. state of New Mexico, and the county seat of Santa Fe County.With over 89,000 residents, [5] Santa Fe is the fourth-most populous city in the state, [6] and part of the Albuquerque–Santa Fe–Los Alamos combined statistical area, which had a population of 1,162,523 in 2020.
Bandelier National Monument is a 33,677-acre (136 km 2) United States National Monument near Los Alamos in Sandoval and Los Alamos counties, New Mexico. The monument preserves the homes and territory of the Ancestral Puebloans of a later era in the Southwest. Most of the pueblo structures date to two eras, dating between AD 1150 and 1600.
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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.