Picuris Pueblo is a historic pueblo in Taos County, New Mexico, United States. It is also a census-designated place (CDP) and a federally recognized tribe of Native American Pueblo people. The 2010 census estimated that 68 people lived in the CDP, while 267 people in the U.S. reported being of the tribal group Picuris alone and 439 reported being of the tribal group Picuris alone or in combination with other groups. Picurís Pueblo is a member of the Eight Northern Pueblos. Their own name for their pueblo is P'įwweltha, meaning "mountain warrior place" or "mountain pass place." They speak the Picuris dialect of the Northern Tiwa language, part of the Kiowa-Tanoan language family.
Questa is a village in Taos County, New Mexico, United States. The population was 1,770 at the 2010 census. The village has trails into the Rio Grande Gorge, trout fishing, and mountain lakes with trails that access the Sangre de Cristo Mountains that overlook the area. Questa is on the Enchanted Circle Scenic Byway, near the confluence of the Rio Grande and the Red River. The "Gateway to the Rio Grande del Norte Monument", its visitors can drive to an overlook of the Red River meeting the Rio Grande in the depth of the gorge. The Carson National Forest parallels Questa to the east. The Columbine Hondo Wilderness and Latir Peak Wildness are in the Carson National Forest close to Questa.
The Sangre de Cristo Mountains are the southernmost subrange of the Rocky Mountains. They are located in southern Colorado and northern New Mexico in the United States. The mountains run from Poncha Pass in South-Central Colorado, trending southeast and south, ending at Glorieta Pass, southeast of Santa Fe, New Mexico. The mountains contain a number of fourteen thousand foot peaks in the Colorado portion, as well as several peaks in New Mexico which are over thirteen thousand feet.
Jicarilla Apache, one of several loosely organized autonomous bands of the Eastern Apache, refers to the members of the Jicarilla Apache Nation currently living in New Mexico and speaking a Southern Athabaskan language. The term jicarilla comes from Mexican Spanish meaning "little basket", referring to the small sealed baskets they used as drinking vessels. To neighboring Apache bands, such as the Mescalero and Lipan, they were known as Kinya-Inde.
Carson National Forest is a national forest in northern New Mexico, United States. It encompasses 6,070 square kilometers and is administered by the United States Forest Service. The Forest Service's "mixed use" policy allows for its use for recreation, grazing, and resource extraction.
The Rio Grande white wares comprise multiple pottery traditions of the prehistoric Puebloan peoples of New Mexico. About AD 750, the beginning of the Pueblo I Era, after adhering to a different and widespread regional ceramic tradition for generations, potters of the Rio Grande region of New Mexico began developing distinctly local varieties of black-on-white pottery. This pottery involved the use of black mineral paint or black vegetal paint on a white, off-white, or light gray background. The black-on-white tradition finally died out about AD 1750.
The 56-mile (90 km) High Road to Taos is a scenic, winding road through the Sangre de Cristo Mountains between Santa Fe and Taos.. It winds through high desert, mountains, forests, small farms, and tiny Spanish land grant villages and Pueblo Indian villages. Scattered along the way are the galleries and studios of traditional artisans and artists drawn by the natural beauty. It has been recognized by the state of New Mexico as an official scenic byway.
The Rio Grande del Norte National Monument is an approximately 242,555-acre (98,159 ha) area of public lands in Taos County, New Mexico, United States, proclaimed as a national monument on March 25, 2013, by President Barack Obama under the provisions of the Antiquities Act. It consists of the Rio Grande Gorge and surrounding lands, managed by the Bureau of Land Management (BLM).
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.
Taos Valley, also called Lower Taos Canyon, is a valley located in Taos County, New Mexico. It is bounded by the Rio Grande Gorge; the deep ravine, or Arroyo Hondo, of the Rio Hondo; and the Taos Mountain range. Included in the valley are Ranchos de Taos, the Taos Pueblo, and Taos Plaza.
The Vadito Group is a group of geologic formations that crops out in most of the Precambrian-cored uplifts of northern New Mexico. Detrital zircon geochronology and radiometric dating give a consistent age of 1700 Mya for the group, corresponding to the Statherian period.
The Burned Mountain Formation is a geologic formation that crops out in the Tusas Mountains of northern New Mexico. It has a U-Pb radiometric age of 1700 Mya, corresponding to the Statherian period.
The Glenwoody Formation is a geological formation that is exposed in the cliffs southeast of the Rio Grande Gorge near the town of Pilar and in a few other locations in the Picuris Mountains. Its minimum age from detrital zircon geochronology is 1.693 Mya, corresponding to the Statherian period.
The Hondo Group is a group of geologic formations that crops out in most of the Precambrian-cored uplifts of northern New Mexico. Detrital zircon geochronology gives a maximum age for the lower Hondo Group of 1765 to 1704 million years (Mya), corresponding to the Statherian period.
The Ortega Formation is a geologic formation that crops out in most of the mountain ranges of northern New Mexico. Detrital zircon geochronology establishes a maximum age for the formation of 1690-1670 million years (Mya), in the Statherian period of the Precambrian.
The Rinconada Formation is a geologic formation that crops out in the Picuris Mountains of northern New Mexico. Detrital zircon geochronology establishes a maximum age for the Rinconada Formation of about 1723 Mya, placing it in the Statherian period of the Precambrian.
The Pilar Formation is a geologic formation that crops out in the Picuris Mountains of northern New Mexico. It has a radiometric age of 1488 ± 6 million years, corresponding to the Calymmian period.
The Marquenas Formation is a geological formation that crops out in the Picuris Mountains of northern New Mexico. Detrital zircon geochronology gives it a maximum age of 1435 million years, corresponding to the Calymmian period.
The Servilleta Basalt or Servilleta Formation is a geologic formation that underlies most of the Taos Plateau of northern New Mexico. It has a radiometric age of 3.6 to 4.5 million years, corresponding to the Pliocene epoch.
The Picuris Formation is a geologic formation exposed in the eastern flank of the Rio Grande rift in northern New Mexico. It was deposited from the late Eocene to Miocene epochs.
