Red River of the South
The Red River, or sometimes the Red River of the South, is a major river in the Southern United States. It was named for the red-bed country of its watershed. It is one of several rivers with that name. Although it was once a tributary of the Mississippi River, the Red River is now a tributary of the Atchafalaya River, a distributary of the Mississippi that flows separately into the Gulf of Mexico. It is connected to the Mississippi River by the Old River Control Structure.
The south bank of the Red River formed part of the US–Mexico border from the Adams–Onís Treaty until the Texas Annexation and the Treaty of Guadalupe Hidalgo.
The Red River is the second-largest river basin in the southern Great Plains. It rises in two branches in the Texas Panhandle and flows east, where it acts as the border between the states of Texas and Oklahoma. It forms a short border between Texas and Arkansas before entering Arkansas, turning south near Fulton, Arkansas, and flowing into Louisiana, where it flows into the Atchafalaya River. The total length of the river is, with a mean flow of over at the mouth.
Geography
Course
The North Fork Red River meets the southern and largest fork near the Texas–Oklahoma border. The southern fork, which is about long, is generally called the Prairie Dog Town Fork. It is formed in Randall County, Texas, near the county seat of Canyon, by the confluence of Tierra Blanca Creek and intermittent Palo Duro Creek.between Oklahoma and Texas, photographed on the Oklahoma side
, and left behind Cane River Lake.
The Red River turns and flows southeast through Palo Duro Canyon in Palo Duro Canyon State Park at an elevation of, then past Newlin, Texas, to meet the Oklahoma state line. Past that point, it is generally considered the main stem of the Red River. Near Elmer, Oklahoma, the North Fork finally joins, and the river proceeds to follow a winding course east through one of the most arid parts of the Great Plains, receiving the Wichita River as it passes the city of Wichita Falls. Near Denison, the river exits the eastern end of Lake Texoma, a reservoir formed by the Denison Dam. The lake is also fed by the Washita River from the north.
s in Lafayette and Miller counties, Arkansas
After the river flows out of the southeastern end of the lake, it runs generally east towards Arkansas and receives Muddy Boggy Creek before turning southward near Texarkana.
Soon after, the waterway crosses south into Louisiana. The sister cities of Shreveport and Bossier City were developed on either bank of the river, as were the downriver cities of Alexandria and Pineville. Where it is joined by the Ouachita River, its largest tributary, the river later broadens into a complex network of marshlands surrounding the Mississippi and Atchafalaya rivers. Its waters eventually discharge into the Atchafalaya River and flow eastward or southward into the Gulf of Mexico.
In 1946, the Red River flood spilled over into Pineville because of insufficient levee height and strength. However, the taller and stronger levee held in Alexandria. Willie E. Kees Jr., the newly elected mayor of Pineville, worked to gain support for the Corps of Engineers to increase the height of the levee on the eastern side of the river to equal that in Alexandria.
Tributaries
Tributaries include the Little Red River, Prairie Dog Town Fork Red River, Salt Fork Red River, North Fork Red River, Pease River, Washita River, Kiamichi River, Wichita River, Little Wichita River, Little River, Sulphur River, Loggy Bayou as well as the Ouachita River not far from the mouth.Saltwater river
The Red River is a saltwater river. The saltiness is caused by a natural phenomenon that dates back to ancient times. About 250 million years ago, an inland sea blanketed parts of what is now those states. As time passed, that sea evaporated, leaving salt deposits – mostly sodium chloride. Rock and silt eventually buried the deposits, but the salt continues to leech through natural seeps in tributaries above Lake Texoma, sending as much as 3,450 tons of salt per day flowing down the Red River.Watershed
The Red River's watershed covers and is the southernmost major river system in the Great Plains. Its drainage basin is mostly in the states of Texas and Oklahoma, but also covers parts of New Mexico, Arkansas and Louisiana. Its basin is characterized by flat, fertile agricultural land, with only a few major cities. The drainage basin of the Red River is very arid and receives little precipitation. As a result, much of the river above the Texas–Oklahoma border is intermittent, and until the river is past its great bend south in Arkansas, the flow varies widely. Most of the agriculture in the basin is sustained by groundwater, which is recharged with rainfall and riverflow. The lower course of the river flows through a series of marshes and swamps, where its flow is dramatically moderated.History
Native Americans
Native American cultures along the river were diverse, developing specialized adaptations to the many different environments. By the time of European contact, the eastern Piney Woods were dominated by the numerous historic tribes of the Caddo Confederacy. They found plentiful game and fish, and also had good land for cultivating staple crops. The middle part of the Red River was dominated by Wichita and Tonkawa. This area was prairie, where Native Americans constructed portable and temporary tepees for housing. They practiced limited farming and followed game in seasonal, nomadic hunting cycles. The Plains division of the Lipan Apache dominated the western Red River area until the 18th century, when they were displaced by invading Comanche from the north.European-American exploration and settlement
In 1806, President Thomas Jefferson commissioned the Red River Expedition to explore parts of the new lands of the Louisiana Purchase by traveling up the Red River. He said it was "in truth, next to the Missouri, the most interesting water of the Mississippi", in a letter to William Dunbar. Having threaded the maze of bayous at the river's confluence, and the "Great Raft" of lodged driftwood, the expedition was stopped by the Spanish near what is now New Boston, Texas.In 1806, Lieutenant Zebulon Pike, under orders to ascertain the source of the Red River, ascended the Arkansas River, made his way downstream on what turned out to be the Rio Grande, and was sent home by the Spanish authorities. A more successful exploration of the river's upper reaches to both its sources was the 1852 expedition under Capt. Randolph Barnes Marcy, assisted by Brevet Capt. George B. McClellan. A decade later McClellan was an important general in the American Civil War.
In April 1815, Captain Henry Miller Shreve was the first person to bring a steamboat, the Enterprise, up the Red River. Fulton and Livingston, who claimed the exclusive right to navigate Louisiana waters by steamboat, sued Shreve in the District Court of New Orleans. The judge ruled that the monopoly claimed by the plaintiffs was illegal. That decision, along with a similar outcome in Gibbons v. Ogden freed navigation on every river, lake or harbor in the United States from interference by monopolies.
When John Quincy Adams became Secretary of State in 1817, one of his highest priorities was to negotiate the boundaries of the Louisiana Purchase with Spain. He negotiated with the Spanish Minister to the United States, Luis de Onis, and finally concluded the Adams–Onis Treaty, also known as the Treaty of 1819. The treaty defined the south bank of the river as the boundary between the United States and Spain. That boundary continued to be recognized when Mexico gained its independence from Spain, then again when Texas became independent from Mexico. It remained so until the United States Congress consented to the Red River Boundary Compact adopted by the states of Oklahoma and Texas, which set the jurisdictional boundary between Texas and Oklahoma at the vegetation line on the south bank, but left title of adjacent property owners at the south bank.
The Red River Campaign was fought along the Red River Valley in Louisiana during the American Civil War. It was a failed attempt by the Union to occupy eastern Texas. Confederate commander Richard Taylor was able to repel an army under Nathaniel Banks three times bigger than his own.
In Louisiana, the area of present-day Natchitoches Parish was settled by French Creole and mixed-race Louisiana Creole people, starting before 1800. The Cane River National Heritage Area marks this area of influence, with plantations and churches founded by Louisiana Creoles. Some of the sites are designated as destinations on the Louisiana African American Heritage Trail, designed in the 21st century. For nearly 100 years after the American Civil War, some of the plantations were the center of a large African American and Creole community, whose people lived and worked in this area for generations.
The area along the lower Red River of Grant Parish, Louisiana and neighboring parishes were a mixture of hill country and cotton plantations, with white planters and subsistence farmers, and numerous African American slaves working the plantations in the ante bellum years. It was an area of heated social tensions and insurgency during and after the Reconstruction era. Grant was a new parish created by the Reconstruction legislature, with the goal of increasing Republican Party representation. In 1873, Grant Parish was the site of the Colfax massacre, caused by political tension and violence arising from the disputed 1872 gubernatorial election and efforts by local whites to maintain white supremacy. White militias, organized from nearby parishes, killed more than 100 freedmen, some of whom had surrendered as prisoners.
In 1874, such militias organized as the White League in Grant Parish and other chapters were soon founded across the state. The Coushatta massacre was attributed to the White League, which attacked Republican office holders to run them out of office. The paramilitary groups intimidated and terrorized freedmen to keep them from the polls, and by the late 1870s, conservative Democrats had retaken political control of the state.
Great Raft
In the early 19th century, settlers found that much of the river's length in Louisiana was unnavigable because of a collection of fallen trees that formed a "Great Raft" over long. Captain Henry Miller Shreve began clearing the log jam in 1839. The log jam was not completely cleared until the 1870s, when dynamite became available. The river was thereafter navigable, but north of Natchitoches it was restricted to small craft. Removal of the raft further connected the Red and Atchafalaya rivers, accelerating the development of the Atchafalaya River channel.In the 20th century, the interest group known as the Red River Valley Association was formed to lobby the United States Congress to make the river fully navigable between Alexandria and Shreveport, Louisiana. Leading supporters of the longstanding project were Louisiana Democratic senators Allen J. Ellender, J. Bennett Johnston and Russell B. Long, the Fourth District Congressman Joe Waggonner, and the late Shreveport Mayor Calhoun Allen. With the completion of the project, a lock system constructed by the US Army Corps of Engineers allowed navigation of barge traffic as far north as Shreveport.