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Cañon Del Muerto (Sierra County, New Mexico)
Cañon del Muerto is a canyon, in Sierra County, New Mexico. The mouth of the Cañon del Muerto, was originally considered to flow into the Rio Grande. Its lower reach was later renamed McRae Canyon, with Cañon del Muerto having its mouth at its confluence with McRae Canyon at at an elevation of , below an unnamed arroyo flowing from the east, at an elevation of . Cañon del Muerto's source is at an elevation of at . History The Ojo del Muerto, an artesian spring, was located at , above the confluence of Cañon del Muerto with an unnamed arroyo that flows into McRae Canyon. It was one of the few reliable water sources along the route of the Jornada del Muerto, although stock and water carriers had to travel several leagues (5 or 6 miles) west from the trail to the spring and back. It was also the water source of the Apache in the region and very risky for travelers to obtain water there. Also the Cañon del Muerto was an easily traveled gap through the mountains between the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sierra County, New Mexico
Sierra County is a county located in the U.S. state of New Mexico. As of the 2020 Census, the population was 11,576. Its county seat is Truth or Consequences. Geography According to the U.S. Census Bureau, the county has a total area of , of which is land and (1.4%) is water. Adjacent counties * Catron County - northwest * Socorro County - north * Lincoln County - northeast * Otero County - east * Doña Ana County - south * Luna County - south * Grant County - west National protected areas * Cibola National Forest (part) * El Camino Real de Tierra Adentro National Historic Trail (part) * Gila National Forest (part) Major highways * * * * * * * Demographics 2000 census As of the 2000 census, there were 13,270 people, 6,113 households, and 3,618 families living in the county. The population density was 3 people per square mile (1/km2). There were 8,727 housing units at an average density of 2 per square mile (1/km2). The racial makeup of the county was 86.9 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rio Grande
The Rio Grande ( and ), known in Mexico as the Río Bravo del Norte or simply the Río Bravo, is one of the principal rivers (along with the Colorado River) in the southwestern United States and in northern Mexico. The length of the Rio Grande is . It originates in south-central Colorado, in the United States, and flows to the Gulf of Mexico. The Rio Grande drainage basin (watershed) has an area of ; however, the endorheic basins that are adjacent to and within the greater drainage basin of the Rio Grande increase the total drainage-basin area to . The Rio Grande with Rio Grande Valley (landform), its fertile valley, along with its tributaries, is a vital watersource for seven US and Mexican states, and flows primarily through arid and semi-arid lands. After traversing the length of New Mexico, the Rio Grande becomes the Mexico–United States border, between the U.S. state of Texas and the northern Mexican states of Chihuahua (state), Chihuahua and Coahuila, Nuevo León a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McRae Canyon
McRae Canyon originally known as Cañon del Muerto, is a canyon in the southern Fra Cristobal Range in Sierra County, New Mexico. Its waters are tributary to the Rio Grande, and today flow into the Elephant Butte Reservoir at the head of an inlet in the flooded lower canyon, at an elevation of . Its source is at , at an elevation of in the southern Fra Cristobal Range. McRae Canyon has one major tributary the Cañon del Muerto that has its confluence with McRae Canyon a short distance below that with an unnamed arroyo at . Just below this confluence is an artesian spring, that flows continuously from the Jornada del Muerto basin aquifer. McRae Canyon is the site of Fort McRae manned by California Volunteers of the Union Army from 1863 to 1866, and by U. S. Army The United States Army (USA) is the land service branch of the United States Armed Forces. It is one of the eight U.S. uniformed services, and is designated as the Army of the United States in the U.S. Constituti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ojo Del Muerto
Ojo del Muerto, (Spring of the Dead Man) was an historical artesian spring in Cañon del Muerto in the southern Fra Cristobal Range nearby to the southeast of the later site of Fort McRae Fort McRae was a Union Army post, established in 1863, then a U.S. Army post from 1866 and closed in 1876, in what is now Sierra County, New Mexico. The post was named for Alexander McRae (1829–1862) a slain hero of the 1862 Battle of Valverde. ... that operated in McRae Canyon from 1863 to 1876. from newmexicohistory.org accessed December 28, 2016. Due to the lowering of the water table by wells drilled for water in the Jornada del Muerto basin since the time of the American Civil War, the old Ojo del Muerto dried up. Lower strata found in McRae Canyon still produce a similar spring just below the conflu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Artesian Aquifer
An artesian aquifer is a confined aquifer containing groundwater under positive pressure. An artesian aquifer has trapped water, surrounded by layers of impermeable rock or clay, which apply positive pressure to the water contained within the aquifer. If a well were to be sunk into an artesian aquifer, water in the well-pipe would rise to a height corresponding to the point where hydrostatic equilibrium is reached. A well drilled into such an aquifer is called an ''artesian well''. If water reaches the ground surface under the natural pressure of the aquifer, the well is termed a ''flowing artesian well''. Fossil water aquifers can also be artesian if they are under sufficient pressure from the surrounding rocks, similar to how many newly tapped oil wells are pressurized. From the previous statement, it can be inferred that not all aquifers are artesian (i.e., water table aquifers occur where the groundwater level at the top of the aquifer is at equilibrium with atmospher ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (hydrology)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jornada Del Muerto
The name Jornada del Muerto translates from Spanish as "Single Day's Journey of the Dead Man" or even "Route of the Dead Man, though the modern literal translation is closer to "The Working Day of the Dead". It was the name given by the Spanish conquistadors to the Jornada del Muerto Desert basin, and the particularly dry stretch of a route through it from Las Cruces to Socorro, New Mexico. The trail led northward from central Spanish colonial New Spain, present-day Mexico, to the farthest reaches of the viceroyalty in northern Nuevo México Province (the area around the upper valley of the Rio Grande). The route later became a section of the Camino Real. Natural history The Jornada del Muerto desert is a wide and long stretch of flat desert landforms and xeric habitat about from north to south. The desert runs between the Oscura Mountains and San Andres Mountains on the east, and the Fra Cristóbal Range and Caballo Mountains on the west. The western mountains block acces ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Apache
The Apache () are a group of culturally related Native American tribes in the Southwestern United States, which include the Chiricahua, Jicarilla, Lipan, Mescalero, Mimbreño, Ndendahe (Bedonkohe or Mogollon and Nednhi or Carrizaleño and Janero), Salinero, Plains (Kataka or Semat or "Kiowa-Apache") and Western Apache ( Aravaipa, Pinaleño, Coyotero, Tonto). Distant cousins of the Apache are the Navajo, with whom they share the Southern Athabaskan languages. There are Apache communities in Oklahoma and Texas, and reservations in Arizona and New Mexico. Apache people have moved throughout the United States and elsewhere, including urban centers. The Apache Nations are politically autonomous, speak several different languages, and have distinct cultures. Historically, the Apache homelands have consisted of high mountains, sheltered and watered valleys, deep canyons, deserts, and the southern Great Plains, including areas in what is now Eastern Arizona, Northern Mexico ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fort McRae
Fort McRae was a Union Army post, established in 1863, then a U.S. Army post from 1866 and closed in 1876, in what is now Sierra County, New Mexico. The post was named for Alexander McRae (1829–1862) a slain hero of the 1862 Battle of Valverde. The site of Fort McRae is located on the east bank of the Elephant Butte Reservoir in the general area of Elephant Butte, New Mexico within McRae Canyon. A area at the site was listed on the National Register of Historic Places in 2005. In National Park Service sources its precise location was . History Union Army Fort McRae was first established by California Volunteers of the Union Army during the American Civil War on April 3, 1863. It was located east of the Rio Grande on the south side of Canyon del Muerto, (now known as McRae Canyon), at an elevation of in the southern Fra Cristobal Range, 3 miles northeast of Elephant Butte, in Sierra County, New Mexico. It was located nearby to the west of the Ojo del Muerto, a spring ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyons And Gorges Of New Mexico
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Sierra 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 the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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