The Brazos River, called the Río de los Brazos de Dios by early Spanish explorers, is the 14th-longest river in the United States at 1,280 miles (2,060 km) from its headwater source at the head of Blackwater Draw, Roosevelt County, New Mexico to its mouth at the Gulf of Mexico with a 45,000-square-mile (116,000 km2) drainage basin. Being one of Texas' largest rivers, it is sometimes used to mark the boundary between East Texas and West Texas.
The Owyhee River is a tributary of the Snake River located in northern Nevada, southwestern Idaho and southeastern Oregon in the United States. It is 280 miles (450 km) long. The river's drainage basin is 11,049 square miles (28,620 km2) in area, one of the largest subbasins of the Columbia Basin. The mean annual discharge is 995 cubic feet per second (28.2 m3/s), with a maximum of 50,000 cu ft/s (1,400 m3/s) recorded in 1993 and a minimum of 42 cu ft/s (1.2 m3/s) in 1954.
The Salt Fork Red River is a sandy-braided stream about 311 km (193 mi) long, heading on the Llano Estacado of West Texas about 2.9 km (1.8 mi) north of Claude of Armstrong County, Texas, flowing east across the Texas Panhandle and Western Oklahoma to join the Red River about 21 km (13 mi) south of Altus of Jackson County, Oklahoma.
Prairie Dog Town Fork Red River is a sandy-braided stream about 120 mi (193 km) long, formed at the confluence of Palo Duro Creek and Tierra Blanca Creek, about 1.8 mi (2.9 km) northeast of Canyon in Randall County, Texas, and flowing east-southeastward to the Red River about 1 mi (2 km) east of the 100th meridian, 8 mi (13 km) south-southwest of Hollis, Oklahoma.
The Pease River is a river in Texas, United States. It is a tributary of the Red River that runs in an easterly direction through West Texas. It was discovered and mapped for the first time in 1856 by Jacob de Córdova, who found the river while surveying for the Galveston, Houston and Henderson Railroad Company; it was named after Texas Governor Elisha M. Pease. In December 1860, the Texas Rangers recaptured Cynthia Ann Parker and her daughter from the Comanche Indians at an engagement along the river.
Croton Creek is an intermittent stream that flows through the Croton Breaks of Dickens, Kent and Stonewall counties in the U.S. state of Texas. It is a tributary of the Salt Fork Brazos River, which eventually merges with the Double Mountain Fork to form the Brazos River.
The White River is an intermittent stream in the South Plains of Texas and a tributary of the Brazos River of the United States. It rises 8 miles (13 km) west of Floydada in southwestern Floyd County at the confluence of Callahan and Runningwater Draws. From there, it runs southeast for 62 miles (100 km) to its mouth on the Salt Fork of the Brazos River in northwestern Kent County. Besides these two headwaters, which rise near Hale Center and in Curry County, New Mexico, respectively, other tributaries include Pete, Crawfish, and Davidson Creeks. The White River drains an area of 1,690 sq mi (4,377 km2).
Mulberry Creek is an intermittent stream about 58 mi (93 km) long, formed as a shallow draw on the high plains of the Llano Estacado in Armstrong County, Texas, and flowing southeastward to join the Prairie Dog Town Fork Red River in Hall County, Texas.
Nolan River is a river in north central Texas, running through Johnson County and Hill County and is part of the Brazos River drainage basin. The Nolan's headwaters are in farm land in northwest Johnson County. The river runs generally parallel to, and about 10 miles (16 km) east of, the Brazos River. The Nolan flows in a southeasterly direction from its headwaters for about 27 miles (43 km) to its confluence with the Brazos River in the headwaters of Lake Whitney in Hill County, south of the town of Blum, Texas.
Sagerton is an unincorporated community in Haskell County, Texas, United States.
The Double Mountain Fork Brazos River is an ephemeral, sandy-braided stream about 170 mi (280 km) long, heading on the Llano Estacado of West Texas about 11.5 mi (18.5 km) southeast of Tahoka, Texas, flowing east-northeast across the western Rolling Plains to join the Salt Fork, forming the Brazos River about 18 mi (29 km) west-northwest of Haskell, Texas.
The North Fork Double Mountain Fork Brazos River is an intermittent stream about 75 mi (121 km) long, heading at the junction of Blackwater Draw and Yellow House Draw in the city of Lubbock, flowing generally southeastward to its mouth on the Double Mountain Fork Brazos River in western Kent County. It crosses portions of Lubbock, Crosby, Garza, and Kent counties in West Texas.
The Rice Fork is a 22.7-mile-long (36.5 km) tributary of the Eel River in Lake County, California. The Rice Fork begins on the upper northwest side of Goat Mountain, on the Colusa-Lake County line, at an elevation of over 6,000 feet (1,800 m). It quickly descends the steep western slope of the mountain, then bends northward, and flows northwesterly down a narrow winding steep walled canyon for about 18 miles (29 km), crossing two forest roads and adding many tributaries, ending its journey at the southern tip of Lake Pillsbury, at a varied elevation around 1,800 feet (550 m), depending on the lake level. Before the construction of Scott Dam in the 1920s, which formed Lake Pillsbury, the Rice Fork ran directly into the Eel River. It is one of Lake County's longest streams.
The Juab Valley is a 40-mile (64 km) long valley located on the eastern edge of Juab County, Utah, United States.
The Salt Fork Brazos River is a braided, highly intermittent stream about 150 mi (240 km) long, heading along the edge of the Llano Estacado about 26 mi (42 km) east-southeast of Lubbock, Texas. From its source, it flows generally east-southeastward to join the Double Mountain Fork to form the Brazos River about 18 mi (29 km) west-northwest of Haskell, Texas. The Salt Fork stretches across portions of Crosby, Garza, Kent, and Stonewall counties of West Texas.
The Rio Brazos is a 42-mile (68 km) long river flowing through northern New Mexico in the United States. It rises in the Tusas Mountains, a subrange of the San Juan Mountains, and runs generally southwest to a confluence with the Rio Chama, part of the larger Rio Grande system.
The Little Red River is an intermittent stream about 30 mi (48 km) long, formed at the confluence of the North Prong and South Prong Little Red River in Briscoe County, Texas, and flowing east-northeastward to join the Prairie Dog Town Fork Red River in Hall County, Texas.
McDonald Creek is an intermittent stream, about 25 mi (40 km) long, heading about 10 mi (16 km) south-southwest of Crosbyton, Texas, and trending generally southeast to join the Salt Fork Brazos River near the community of Verbena, Texas.
Quitaque Creek is an intermittent stream about 40 mi (64 km) long, originating as a shallow draw on the high plains of the Llano Estacado in Floyd County, Texas, and flowing eastward to join the North Pease River in Motley County, Texas.
