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Cerro Pedernal
Cerro Pedernal, locally known as just "Pedernal", is a narrow mesa in northern New Mexico. The name is Spanish for "flint hill". The mesa lies on the north flank of the Jemez Mountains, south of Abiquiu Lake, in the Coyote Ranger District of the Santa Fe National Forest. Its caprock was produced in the Jemez Volcanic Field. Its highest point is at . Pedernal is the source of a chert used by the prehistoric Gallina people. Its cliffs are popular with rock climbers. Georgia O'Keeffe Georgia Totto O'Keeffe (November 15, 1887 – March 6, 1986) was an American modernist artist. She was known for her paintings of enlarged flowers, New York skyscrapers, and New Mexico landscapes. O'Keeffe has been called the "Mother of Ame ... made many paintings of it, and her ashes were scattered on its top. References External links Cerro Pedernal review with photos Climb.Mountains.com. New Mexico Bureau of Geology and Mineral Resources. * Jemez Mountains Landforms of Rio Arri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ghost Ranch
Ghost Ranch is a retreat and education center located close to the village of Abiquiú in Rio Arriba County in north central New Mexico, United States. It was the home and studio of Georgia O'Keeffe, as well as the subject of many of her paintings. Ghost Ranch is also known for a remarkable concentration of fossils, most notably that of the theropod dinosaur ''Coelophysis'', of which it has been estimated that nearly a thousand individuals have been preserved in a quarry at Ghost Ranch. History Ghost Ranch is part of Piedra Lumbre (Spanish, "Shining Rock"), a 1766 land grant to Pedro Martin Serrano from Charles III of Spain. The Rito del Yeso is a stream that meanders through the canyons and gorge, providing a drought-resistant source of water for life to thrive. In 1976, Ghost Ranch was designated as a National Natural Landmark by the National Park Service. The canyon was first inhabited by the Archuleta brothers, cattle rustlers who enjoyed the coverage and invisibility tha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jemez Volcanic Field
The Jemez Mountains are a group of mountains in Rio Arriba, Sandoval, and Los Alamos counties, New Mexico, United States. Numerous Puebloan Indian tribes have lived in the Jemez Mountains region since before the Spanish arrived in New Mexico. The Pueblo Indians of this region are the Towa-speaking Jemez people for which this mountain range is named, the Keres-speaking Keresan Indians, and the Tewa-speaking Tewa Indians. Tsąmpiye'ip'įn is the Tewa language name for the Jemez Mountains. The highest point in the range is Chicoma Mountain (also spelled as Tschicoma or Tchicoma) at an elevation of . The town of Los Alamos and the Los Alamos National Laboratory adjoin the eastern side of the range while the town of Jemez Springs is to the west. Pajarito Mountain Ski Area is the only ski area in the Jemez. New Mexico State Highway 4 is the primary road that provides vehicular access to locations in the Jemez Mountains. Geology The Jemez Mountains lie to the north of the Albuq ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesas Of New Mexico
A mesa is an isolated, flat-topped elevation, ridge or hill, which is bounded from all sides by steep escarpments and stands distinctly above a surrounding plain. Mesas characteristically consist of flat-lying soft sedimentary rocks capped by a more resistant layer or layers of harder Rock (geology), rock, e.g. shales overlain by sandstones. The resistant layer acts as a caprock that forms the flat summit of a mesa. The caprock can consist of either sedimentary rocks such as sandstone and limestone; dissected lava flows; or a deeply eroded duricrust. Unlike ''plateau'', whose usage does not imply horizontal layers of bedrock, e.g. Tibetan Plateau, the term ''mesa'' applies exclusively to the landforms built of flat-lying strata. Instead, flat-topped plateaus are specifically known as ''Table (landform), tablelands''.Duszyński, F., Migoń, P. and Strzelecki, M.C., 2019. ''Escarpment retreat in sedimentary tablelands and cuesta landscapes–Landforms, mechanisms and patterns.'' '' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Rio Arriba County, New Mexico
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Youngsville, New Mexico
Youngsville is a census-designated place in Rio Arriba County, New Mexico, United States. Its population was 56 as of the 2010 census. Youngsville has a post office with ZIP code 87064. New Mexico State Road 96 State Road 96 (NM 96) is a state highway in Sandoval and Rio Arriba counties in New Mexico, United States, that connects U.S. Route 550 (US 550) northwest of Cuba with U.S. Route 84 (US 84) east of Abiquiu Reservoir. Route descr ... passes through the community. Demographics References Census-designated places in New Mexico Census-designated places in Rio Arriba County, New Mexico {{NewMexico-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North American Monsoon
The North American monsoon, variously known as the Southwest monsoon, the Mexican monsoon, the New Mexican monsoon, or the Arizona monsoon is a pattern of pronounced increase in thunderstorms and rainfall over large areas of the southwestern United States and northwestern Mexico, typically occurring between June and mid-September. During the monsoon, thunderstorms are fueled by daytime heating and build up during the late afternoon and early evening. Typically, these storms dissipate by late night, and the next day starts out fair, with the cycle repeating daily. The monsoon typically loses its energy by mid-September when much drier conditions are reestablished over the region. Geographically, the North American monsoon precipitation region is centered over the Sierra Madre Occidental in the Mexican states of Sinaloa, Durango, Sonora and Chihuahua. Mechanism The North American monsoon is a complex weather process that brings moisture from the Gulf of California (and to le ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coyote, Rio Arriba County, New Mexico
Coyote is a village in Rio Arriba County, New Mexico, United States. Its population was 128 as of the 2010 census. Coyote has a post office with ZIP code 87012, a store, a gas station and a school. New Mexico State Road 96 passes through the community. Coyote was settled in 1862. The village is part of a larger census-designated place A census-designated place (CDP) is a concentration of population defined by the United States Census Bureau for statistical purposes only. CDPs have been used in each decennial census since 1980 as the counterparts of incorporated places, such ... which is named after it. References Census-designated places in New Mexico Census-designated places in Rio Arriba County, New Mexico {{NewMexico-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Georgia O'Keeffe
Georgia Totto O'Keeffe (November 15, 1887 – March 6, 1986) was an American modernist artist. She was known for her paintings of enlarged flowers, New York skyscrapers, and New Mexico landscapes. O'Keeffe has been called the "Mother of American modernism". In 1905, O'Keeffe began art training at the School of the Art Institute of Chicago and then the Art Students League of New York. In 1908, unable to fund further education, she worked for two years as a commercial illustrator and then taught in Virginia, Texas, and South Carolina between 1911 and 1918. She studied art in the summers between 1912 and 1914 and was introduced to the principles and philosophies of Arthur Wesley Dow, who created works of art based upon personal style, design, and interpretation of subjects, rather than trying to copy or represent them. This caused a major change in the way she felt about and approached art, as seen in the beginning stages of her watercolors from her studies at the University of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gallina
The Gallina or Largo-Gallina culture was an occupation sequence during the pre-Spanish colonization of the Americas, Hispanic period in the American Southwest from approximately 1050 to 1300. The culture was located in north-central New Mexico roughly north of the Jemez Mountains, and was named after the Rio Gallina (and Largo Canyon), which runs through the region. Ancestry The Gallina are tentatively linked to the Rosa Phase of the Ancestral Puebloans.Ford et al. 1972 Evidence indicates a connection to the Rosa people, due to similar skills such as basket weaving, black on white pottery, and architecture. They also have similar ornaments such as shells pierced for stringing, bone beads, and stone pipes. Tools and artifacts Artifact (archaeology), Artifacts from the Gallina time period are often hard to classify. For example, what archeologists originally classified as Scraper (archaeology), scrapers later proved to be knives. Frequently, assessing an object itself is not en ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chert
Chert () is a hard, fine-grained sedimentary rock composed of microcrystalline or cryptocrystalline quartz, the mineral form of silicon dioxide (SiO2). Chert is characteristically of biological origin, but may also occur inorganically as a precipitation (chemistry), chemical precipitate or a diagenesis, diagenetic replacement, as in petrified wood. Chert is typically composed of the petrified remains of siliceous ooze, the biogenic sediment that covers large areas of the deep ocean floor, and which contains the silicon skeletal remains of diatoms, Dictyochales, silicoflagellates, and radiolarians. Precambrian cherts are notable for the presence of fossil cyanobacteria. In addition to Micropaleontology, microfossils, chert occasionally contains macrofossils. However, some chert is devoid of any fossils. Chert varies greatly in color (from white to black), but most often manifests as gray, brown, grayish brown and light green to rusty redW.L. Roberts, T.J. Campbell, G.R. Rapp Jr. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caprock
Caprock or cap rock is a more resistant rock type overlying a less resistant rock type,Kearey, Philip (2001). ''Dictionary of Geology'', 2nd ed., Penguin Reference, London, New York, etc., p. 41.. . analogous to an upper crust on a cake that is harder than the underlying layer. Description The Niagara Escarpment, over which Niagara Falls flows, is an example of a scarp or escarpment. At Niagara Falls, the caprock is the riverbed above the falls, and is what prevents the river from eroding the face of the falls very quickly. In the photo, the dark thin layer in the foreground where water is not yet running, is the caprock. The Niagara caprock is made of dolomitic limestone. Other common types of caprock are sandstone and mafic rock. In processes such as scarp retreat, the caprock controls the rate of erosion of the scarp. As the softer rock is cut away, periodically the caprock shears off. Caprock is also found in salt domes and on the top of mesa formations. Petroleum In the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rio Arriba County, New Mexico
Rio Arriba County is a county in the U.S. state of New Mexico. As of the 2010 census, the population was 40,246. Its county seat is Tierra Amarilla. Its northern border is the Colorado state line. Rio Arriba County comprises the Española, NM Micropolitan Statistical Area, which is also included in the Albuquerque- Santa Fe-Las Vegas, NM Combined Statistical Area. History The county was one of nine originally created for the Territory of New Mexico in 1852. Originally extending west to the California line, it included the site of present-day Las Vegas, Nevada. The county seat was initially sited at San Pedro de Chamita, and shortly afterwards at Los Luceros. In 1860 the seat was moved to Plaza del Alcalde. Since 1880 Tierra Amarilla has been the county seat. The Battle of Embudo Pass took place in the southern part of the county during the Mexican–American War in January 1847. Geography According to the U.S. Census Bureau, the county has a total area of , of which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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