CONCHO RIVER. The Concho River rises in three branches known as the North Concho, the Middle Concho, and the South Concho. The North Concho, the main branch and a perennial stream, originates two miles north of the Glasscock county line in southern Howard County (at 31°07' N, 101°24' W) and flows southeast for eighty-eight miles across Glasscock, Sterling, Coke, and Tom Green counties to its confluence with the South and Middle Concho rivers, a mile north of Goodfellow Air Force Base in central Tom Green County (at 32°27' N, 100°27' W). The three forks become known as the Concho River at this juncture. San Angelo Dam, which became known as O. C. Fisher Dam (see O. C. FISHER LAKE) was completed on the North Concho in 1951. The Middle Concho rises in southern Sterling County (at 31°38' N, 101°13' W) and runs south and then east for sixty-four miles through Irion County to Twin Buttes Reservoir in western Tom Green County and then to its mouth on Lake Nasworthy (at 31°23' N, 100°31' W). The South Concho rises half a mile east of U.S. Highway 277 in central Schleicher County (at 30°51' N, 100°35' W) and flows north for thirty-six miles through Twin Buttes Reservoir, which was built on the branch in 1963, and Lake Nasworthy, which was completed in 1930, to its confluence with the North Concho River (at 31°27' N, 100°25' W). The consolidated Concho River flows east for fifty-eight miles across Tom Green and Concho counties to its mouth on the Colorado River, one-half mile west of the Coleman county line and one mile south of the Runnels county line in eastern Concho County (at 31°34' N, 99°43' W). Along its route it is joined by fifteen tributaries. Construction of the Simon W. Freeze Dam on the Colorado River, sixteen miles below the confluence of the Colorado and Concho, and the O. H. Ivie Reservoir (formerly Stacy Dam and Reservoir) has flooded the lower reaches of the Concho; water in the reservoir was impounded in 1990. The Concho River and its branches traverse a 246-mile path, crossing caliche beds and wash deposits on flat and rolling terrain, dissecting massive limestone, and ending on steep slopes and benches of limestone and marl. The surrounding soils are generally dark and calcareous stony clays and loams, dark brown to red-brown calcareous sandy clays and loams, and red-brown to gray-brown sandy and clay loams. Vegetation along the river consists primarily of water-tolerant hardwoods and conifers, grasses, scrub brush, creosote bush, cacti, oak, juniper, and mesquite.
The river is named for Spanish concha, "shell." When Hernán Martín and Diego del Castilloqqv explored the area in 1650, they found large quantities of mussel shells that yielded freshwater pearls. Their report was so enthusiastic that Diego de Guadalajara returned to the area four years later; unfortunately, the yield proved to be only about one decent pearl per 100 mussels, and any notion of systematic harvesting was abandoned. Although the river was first called Río de las Nueces because of the many pecans found in the area, the name Concho became the most widely used by the mid-nineteenth century. Some of the best-known Indian pictographs in Texas are found on bluffs along the Concho a mile west of Paint Rock. The river attracted many early Indian tribes, but the Comanches controlled it by the mid-1800s. In 1862 or 1863 John S. Chisum established a ranch on the Concho near its confluence with the Colorado. Fort Concho, a military installation designed to protect travelers and settlers from Indian attack, was established in 1867 at the confluence of the North Concho and the combined Middle and South branches, which offered a steady supply of water.
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The following, adapted from the Chicago Manual of Style, 15th edition, is the preferred citation for this article.Handbook of Texas Online, Julia Cauble Smith, "Concho River," accessed December 08, 2016, http://www.tshaonline.org/handbook/online/articles/rnc12.
Uploaded on June 12, 2010. Published by the Texas State Historical Association.