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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] |
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] |
Fra Cristobal Range
The Fra Cristobal Range, (Fra Cristóbal Range) is a 17 mi (27 km) long, mountain range in central-north Sierra County, New Mexico. Its northern extreme above Fra Cristoblal Mountain extends into Socorro County. The range borders the eastern shore of Elephant Butte Reservoir on the Rio Grande, and the range lies towards the southwest of the Jornada del Muerto, the desert region east of the river. Description The Fra Cristobal Range is an arid, moderate elevation, north–south trending mountain range, about 17 mi long and narrow, only about 7 mi at its widest. Crater Hill, lies west of the central ridgeline, and north of Black Bluffs, Red Cliff at the Reservoir. The high peak in the northern end of the range, which gives the range its name, is Fra Cristobal Mountain, , is at the north perimeter of the range. It is located at The mountain is said to have resembled the profile of a priest, Fray Cristóbal de Salazar, a cousin of Juan de Oñate Juan de O ... [...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] |
Elephant Butte Reservoir
Elephant Butte Reservoir is a reservoir on the southern part of the Rio Grande in the U.S. state of New Mexico, north of Truth or Consequences. The reservoir is the 84th largest man-made lake in the United States and the largest in New Mexico by total surface area and peak volume. It is the only place in New Mexico that one can find pelicans perched on or alongside the lake. There are also temporary US Coast Guard bases stationed at Elephant Butte. It is impounded by Elephant Butte Dam and is part of the largest state park in New Mexico, Elephant Butte Lake State Park. The reservoir is part of the Rio Grande Project to provide power and irrigation to south-central New Mexico and western Texas. It began to be filled in 1915 and 1916 and at highstand was the largest man-made lake in the world. The reservoir can hold of water from a drainage of 28,900 square miles (74,850 km2). It provides irrigation to 178,000 acres (720 km2) of land. Fishing is a popular recreational a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inlet
An inlet is a (usually long and narrow) indentation of a shoreline, such as a small arm, bay, sound, fjord, lagoon or marsh, that leads to an enclosed larger body of water such as a lake, estuary, gulf or marginal sea. Overview In marine geography, the term "inlet" usually refers to either the actual channel between an enclosed bay and the open ocean and is often called an "entrance", or a significant recession in the shore of a sea, lake or large river. A certain kind of inlet created by past glaciation is a fjord, typically but not always in mountainous coastlines and also in montane lakes. Multi-arm complexes of large inlets or fjords may be called sounds, e.g., Puget Sound, Howe Sound, Karmsund (''sund'' is Scandinavian for "sound"). Some fjord-type inlets are called canals, e.g., Portland Canal, Lynn Canal, Hood Canal, and some are channels, e.g., Dean Channel and Douglas Channel. Tidal amplitude, wave intensity, and wave direction are all factors that in ... [...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] |
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] |
California Volunteers
California State Volunteer Units 1861 – 1866 The following are California State Volunteer Units that were active between 1861 – 1866 serving in the Union Army, most west of the Rocky Mountains in place of Federal troops: California Brigade In 1861 four infantry regiments were recruited in Pennsylvania by Californian Senator Edward D. Baker. Though made up of Pennsylvanians they were attributed to California. After the Battle of Ball's Bluff in October 1861 the brigade was renamed Philadelphia Brigade and the regiments were attributed to Pennsylvania as well. *1st California Infantry Regiment - 71st Pennsylvania Infantry Regiment *2nd California Infantry Regiment - 69th Pennsylvania Infantry Regiment *3rd California Infantry Regiment - 72nd Pennsylvania Infantry Regiment *5th California Infantry Regiment - 106th Pennsylvania Infantry Regiment State militia * California State Militia units See also *California Civil War Confederate Units *Lists of American Civil War Re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
