Comanche Springs | |
---|---|
Name origin | Awache (Wide Water) |
Location | Fort Stockton, Pecos County, Texas |
Coordinates | 30°52′54″N102°52′44″W / 30.88167°N 102.87889°W |
Spring source | Edwards Aquifer |
Elevation | 2,940 feet (896.1 m) |
Type | Artesian aquifer |
Provides water for | Rio Grande |
Comanche Springs was an aquifer of six artesian springs geographically located between the Edwards Plateau and the Trans-Pecos regions of West Texas. [1] [2] The military fortification Camp Stockton was built around the springs, eventually growing become the city of Fort Stockton.
The groundwater source originated from a Comanchean limestone fault combined within the bountiful Edwards Aquifer and the Glass Mountains. [3] [4] The natural spring has a physical geography routing north through Comanche Creek forming a confluence with Leon Creek and the Pecos River. [5] The alluvial river is a tributary to the Rio Grande.
Comanche Springs served as an oasis with inhabitants dating to the Pre-Columbian era by the Jumano Indians. [6] Álvar Núñez Cabeza de Vaca scouted the Rio Grande region in 1536. [7] Fernando del Bosque explored the Rio Grandé area for Franciscans missionary districts in 1675 while Juan Domínguez de Mendoza lodged near the spring waters in the late 17th century. [8] [9] [10]
On March 23, 1859, the Camp Stockton fortification was established in the Trans-Pecos region. [11] [12] The garrison served as cantonment for the United States Cavalry warding off Plains Indians seeking to disrupt and raid the American pioneer, Butterfield Overland Mail, Concord stagecoach, covered wagon, Old San Antonio Road, Old Spanish Trail, San Antonio-El Paso Road, San Antonio–San Diego Mail Line, and wagon trains. [13] [14] [15] [16] [17]
The Apache, Comanche, and Kiowa visited the water basin frequently during bison and Colonial Spanish horse hunts, Comanche-Mexico War skirmishes, and Mexican Indian Wars in Northern Mexico. [18] The Comanche Trail permitted the nomadic migration of Native Americans to the West Texas desert climate during the northern hemisphere winter solstice. [19] The long-distance trail encompassed regional spring waters of Texas Big Bend Country given the horseback riding distance from the Staked Plains to Big Spring, Horsehead Crossing, Tunas Springs, Glenn Springs, San Vicente, Las Moras Springs, and Rio Grandé located within Big Bend National Park.
Beginning in 1875, Comanche Springs was incorporated into an agricultural irrigation district resulting in the hydrological regression of the natural springs in the Chihuahuan Desert domain. [20] The Belding territory, located 11 miles (18 km) southwest of Comanche Springs, was a thriving agricultural development requiring voluminous water reserves. [21] The 6,000 acres (2,400 ha) to 7,000 acres (2,800 ha) irrigation demand lead to the overdrafting of the natural springs aquifer diminishing the Trans-Pecos water table. [22]
U.S. Congressional legislation for irrigation of the State of Texas arid lands.
Date of Enactment | Public Law Number | U.S. Statute Citation | U.S. Legislative Bill | U.S. Presidential Administration |
---|---|---|---|---|
June 12, 1906 | P.L. 59-225 | 34 Stat. 259 | H.R. 14184 | Theodore Roosevelt |
August 11, 1916 | P.L. 64-196 | 39 Stat. 506a | H.R. 12365 | Woodrow Wilson |
October 6, 1917 | Public Resolution 65-14 | 40 Stat. 426 | S.J.Res. 89 | Woodrow Wilson |
June 18, 1926 | P.L. 69-404 | 44 Stat. 753 | H.R. 3862 | Calvin Coolidge |
May 28, 1928 | P.L. 70-556 | 45 Stat. 785 | H.R. 11471 | Calvin Coolidge |
February 20, 1958 | P.L. 85-333 | 72 Stat. 17 | S.J.Res. 39 | Dwight Eisenhower |
Comanche Springs received a Texas historic marker in 1968. [23]
Reeves County is a county located in the U.S. state of Texas. As of the 2020 census, its population was 14,748. Its county seat and most populous city is Pecos. The county was created in 1883 and organized the next year. It is named for George R. Reeves, a Texas state legislator and colonel in the Confederate Army. It is one of the nine counties that comprise the Trans-Pecos region of West Texas. Reeves County comprises the Pecos micropolitan statistical area.
Pecos County is a county located in the U.S. state of Texas. As of the 2020 census, its population was 15,193. The county seat is Fort Stockton. The county was created in 1871 and organized in 1875. It is named for the Pecos River. It is one of the nine counties that comprise the Trans-Pecos region of West Texas.
Hudspeth County is a county located in the U.S. state of Texas. As of the 2020 census, the population was 3,202. Its county seat is Sierra Blanca, and the largest community is Fort Hancock. The county is named for Claude Benton Hudspeth, a state senator and United States Representative from El Paso. It is northeast of the Mexico–U.S. border.
Culberson County is a county located in the U.S. state of Texas. As of the 2020 census, its population was 2,188. The county seat is Van Horn. Culberson County was founded in 1911 and organized the next year. It is named for David B. Culberson, a lawyer and Confederate soldier in the American Civil War.
Brewster County is a county located in the U.S. state of Texas. It is in West Texas and its county seat is Alpine. It is one of the nine counties that comprise the Trans-Pecos region, and borders Mexico. Brewster County is the largest county by area in the state - at 6,192 square miles (16,040 km2) it is over three times the size of the state of Delaware, and more than 500 square miles (1,300 km2) bigger than Connecticut.
Fort Stockton is a city in and the county seat of Pecos County, Texas, United States. It is located on Interstate 10, future Interstate 14, U.S. Highways 67, 285, and 385, and the Santa Fe Railroad, 329 mi (529 km) northwest of San Antonio and 240 mi (390 km) southeast of El Paso. Its population was 8,466 at the 2020 census.
The Pecos River originates in north-central New Mexico and flows into Texas, emptying into the Rio Grande. Its headwaters are on the eastern slope of the Sangre de Cristo mountain range in Mora County north of Pecos, New Mexico, at an elevation of over 12,000 feet (3,700 m). The river flows for 926 miles (1,490 km) before reaching the Rio Grande near Del Rio. Its drainage basin encompasses about 44,300 square miles (115,000 km2).
The Edwards Plateau is a geographic region forming the crossroads of Central, South and West Texas, United States. It is bounded by the Balcones Fault to the south and east; the Llano Uplift and the Llano Estacado to the north; and the Pecos River and Chihuahuan Desert to the west. San Angelo, Austin, San Antonio and Del Rio roughly outline the area. The plateau, especially its southeast portion, is also known as the Texas Hill Country.
The Llano Estacado, sometimes translated into English as the Staked Plains, is a region in the Southwestern United States that encompasses parts of eastern New Mexico and northwestern Texas. One of the largest mesas or tablelands on the North American continent, the elevation rises from 3,000 feet (900 m) in the southeast to over 5,000 feet (1,500 m) in the northwest, sloping almost uniformly at about 10 feet per mile (2 m/km).
The Trans-Pecos, as originally defined in 1887 by the Texas geologist Robert T. Hill, is the distinct portion of Texas that lies west of the Pecos River. The term is considered synonymous with Far West Texas, a subdivision of West Texas. The Trans-Pecos is part of the Chihuahuan Desert, the largest desert in North America. It is the most mountainous and arid portion of the state, and most of its vast area is sparsely populated. Among the nine counties in the region are the five largest counties by area in Texas and eight of the eleven largest in the state. The area is known for the natural environment of the Big Bend and the gorge of the Rio Grande, part of which has been designated a National Wild and Scenic Rivers System. With the notable exceptions of Big Bend Ranch State Park, Big Bend National Park and the Guadalupe Mountains National Park, the vast majority of the Trans-Pecos region consists of privately owned ranchland. However, most of the region's population reside in the El Paso metropolitan area. Besides El Paso and its metropolitan area, the major cities are Pecos (12,916), Fort Stockton (8,466), and Alpine (6,035). All other settlements have under 5,000 people.
The Suma were an Indigenous people of Aridoamerica. They had two branches, one living in the northern part of the Mexican state of Chihuahua and the other living near present-day El Paso, Texas. They were semi-nomadic hunter-gatherers who practiced little or no agriculture. The Suma merged with Apache groups and the mestizo population of northern Mexico, and are extinct as a distinct people.
Boquillas was a small settlement in Texas, United States, located on the northern banks of the Rio Grande. It was located within Brewster County, five miles (8 km) northeast of San Vicente. The place existed to service the mining operations at Boquillas del Carmen, Mexico, just across the Rio Grande.
The Comanche Springs pupfish is a species of pupfish in the family Cyprinodontidae. It is endemic to Texas, and is now found only in spring-fed pools near Balmorhea, a small town in West Texas.
Candelaria is an unincorporated community in Presidio County, Texas, United States, with approximately 75 inhabitants.
Horsehead Crossing is a ford on the Pecos River in Crane County, south of Odessa, Texas. Historically, it was a major landmark on the trail west as one of a few fordable sections of the Pecos in West Texas, and as the first reliable source of water for about 75 miles on the route from the east.
The San Antonio–El Paso Road, also known as the Lower Emigrant Road or Military Road, was an economically important trade route between the Texas cities of San Antonio and El Paso between 1849 and 1882. Mail, freight, and passengers traveled by horse and wagon along this road across the Edwards Plateau and dangerous Trans-Pecos region of West Texas.
Glenn Springs is an uninhabited place in the state of Texas, United States, which is of historical importance. The Glenn Springs area was a natural spring providing water for Apache and Kiowa routing the Grand Indian Crossing passage at Boquillas. The Comanche tribes beseech the fresh water crossing on the Comanche Trail during their equine incursions from and to the Mexican Plateau, Sierra Madre Oriental, and the Trans-Mexican Volcanic Belt regions of Mexico.
The Comanche Trail, sometimes called the Comanche War Trail or the Comanche Trace, was a travel route in Texas established by the nomadic Comanche and their Kiowa and Kiowa Apache allies. Although called a "trail," the Comanche Trail was actually a network of parallel and branching trails, always running from one source of good water to another. The trail was especially important from the 1830s to 1850s when the Comanche launched large scale raids from Texas into Mexico. Hundreds of warriors annually followed the trail southward in fall and returned with their booty, mostly livestock, in late winter or spring.
Pecos Spring is a spring, 1.1 miles (3 km) northeast of Sheffield, in Pecos County, Texas. It lies at an elevation of 2060 feet. Pecos Spring was emitted from the Edwards and associated limestones of the Edwards-Trinity (Plateau) aquifer. On March 7, 1924, it discharged 0.7 cubic feet per second but by August 17, 1943, that had been reduced to 0.5 cubic feet per second. By 1961, its flow had ceased.
Pilares was a village located in northwest Presidio County, Texas, United States, on the southern boundary of the Sierra Vieja near the Rio Grande. The river village was 1.25 miles (2.01 km) south of the confluence of Quinn Creek and the Rio Grande while bearing 1.5 miles (2.4 km) north of Porvenir, Texas. The uninhabited site is in the Trans-Pecos region of West Texas with a southern panorama of the Chihuahuan Desert and northern Mexico.