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The State Bar of New Mexico first met on January 19, 1886, in Santa Fe, New Mexico, [2] as a voluntary professional organization. There were 29 original members, and William A. Vincent was the first president. [3] In 1925, state statute caused the State Bar to operate as an agency of the New Mexico Supreme Court.
The state's Mississippian flora of New Mexico included horsetails and scale trees. [5] Pennsylvanian New Mexico experienced both marine and terrestrial conditions over time. [ 5 ] Marine life included more than 157 species of brachiopods, 41 bryozoans, 34 cephalopods, 34 corals, 118 foraminiferans, 87 gastropods, 25 ostracods and 85 pelecypods.
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 ...
Website. nmnaturalhistory.org. The New Mexico Museum of Natural History and Science is a natural history and science museum in Albuquerque, New Mexico near Old Town Albuquerque. The Museum was founded in 1986. [ 1 ] It operates as a public revenue facility of the New Mexico Department of Cultural Affairs.
December 2, 1974 [2] Designated NMSRCP. February 28, 1975. The Zuni-Cibola Complex is a collection of prehistoric and historic archaeological sites on the Zuni Pueblo in western New Mexico. It comprises Hawikuh, Yellow House, Kechipbowa, and Great Kivas, all sites of long residence and important in the early Spanish colonial contact period.
Coelacanth. Coelacanths (/ ˈsiːləkænθ / ⓘ SEE-lə-kanth) (order Coelacanthiformes) are an ancient group of lobe-finned fish (Sarcopterygii) in the class Actinistia. [2][3] As sarcopterygians, they are more closely related to lungfish and tetrapods (which includes amphibians, reptiles, birds and mammals) than to ray-finned fish.
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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.