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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 ...
Life restoration of a herd of Mammuthus columbi, or Columbian mammoths. The extent of the fur depicted is hypothetical. Charles R. Knight (1909). Life restoration of a herd of Neohipparion. Robert Bruce Horsfall (1913). Restoration of a herd of alarmed Miocene-Pleistocene peccaries of the genus Platygonus.
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 ...
The fossil record of North Carolina spans from Eocambrian remains that are 600 million years old, to the Pleistocene 10,000 years ago. About 600 million years ago, North Carolina was covered by a warm shallow sea that was home to corals, jellyfish, and Pteridinium. This sea remained in place during the early part of the Paleozoic era and was ...
Astarte – tentative report. † Asteracanthus. † Atreipus. † Baena – tentative report. † Baikuris – report made of unidentified related form or using admittedly obsolete nomenclature. Barbatia. Fossilized guard of the Late Cretaceous belemnoid cephalopod Belemnitella. † Belemnitella. † Belemnitella americana.
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.
The Taconic orogeny was a mountain building period that ended 440 million years ago (Ma) and affected most of modern-day New England. A great mountain chain formed from eastern Canada down through what is now the Piedmont of the east coast of the United States. As the mountain chain eroded in the Silurian and Devonian periods, sediment spread ...
The cave was discovered in 1936. [5] The site was excavated in the 1930s and 1940s by Frank Hibben while at the University of New Mexico. [6] [7] He claimed to have found the oldest known evidence of humans in the new world, and found a new culture, whose artifacts resembled those of western Europeans, strongly suggesting the first inhabitants of the Americas were Europeans and not far eastern ...