Red River of the South

Last updated
Red River
Rivière Rouge (former French name), Río Colorado (former Spanish name)
Redriverbonhamtx.jpg
Red River looking east, north of Bonham, Texas: Texas is to the right, Oklahoma is on the left, and the border between the two states runs along the south (right) bank of the river.
Redrivermap1.jpg
Map of the Red River watershed
Native nameBah'hatteno [1]
Location
Country United States
States Texas, Oklahoma, Arkansas and Louisiana
Physical characteristics
Source 
 - location Harmon County, Oklahoma
 - coordinates 34°34′35″N99°57′54″W / 34.57639°N 99.96500°W / 34.57639; -99.96500
 - elevation1,535 ft (468 m)
Mouth  
 - location
Atchafalaya River
 - coordinates
31°01′10″N91°44′52″W / 31.01944°N 91.74778°W / 31.01944; -91.74778 Coordinates: 31°01′10″N91°44′52″W / 31.01944°N 91.74778°W / 31.01944; -91.74778
 - elevation
30 ft (9.1 m)
Length1,360 mi (2,190 km)
Basin size65,595 sq mi (169,890 km2)
Discharge 
 - locationmouth; max and min at Alexandria, LA
 - average57,000 cu ft/s (1,600 m3/s)
 - minimum1,472 cu ft/s (41.7 m3/s)
 - maximum233,000 cu ft/s (6,600 m3/s)

The Red River, or sometimes the Red River of the South, is a major river in the southern United States of America. [2] 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.

United States Federal republic in North America

The United States of America (USA), commonly known as the United States or America, is a country comprising 50 states, a federal district, five major self-governing territories, and various possessions. At 3.8 million square miles, the United States is the world's third or fourth largest country by total area and is slightly smaller than the entire continent of Europe's 3.9 million square miles. With a population of over 327 million people, the U.S. is the third most populous country. The capital is Washington, D.C., and the largest city by population is New York City. Forty-eight states and the capital's federal district are contiguous in North America between Canada and Mexico. The State of Alaska is in the northwest corner of North America, bordered by Canada to the east and across the Bering Strait from Russia to the west. The State of Hawaii is an archipelago in the mid-Pacific Ocean. The U.S. territories are scattered about the Pacific Ocean and the Caribbean Sea, stretching across nine official time zones. The extremely diverse geography, climate, and wildlife of the United States make it one of the world's 17 megadiverse countries.

Red beds

Red beds are sedimentary rocks, which typically consist of sandstone, siltstone, and shale that are predominantly red in color due to the presence of ferric oxides. Frequently, these red-colored sedimentary strata locally contain thin beds of conglomerate, marl, limestone, or some combination of these sedimentary rocks. The ferric oxides, which are responsible for the red color of red beds, typically occur as a coating on the grains of sediments comprising red beds. Classic examples of red beds are the Permian and Triassic strata of the western United States and the Devonian Old Red Sandstone facies of Europe.

Drainage basin Area of land where precipitation collects and drains off into a common outlet

A drainage basin is any area of land where precipitation collects and drains off into a common outlet, such as into a river, bay, or other body of water. The drainage basin includes all the surface water from rain runoff, snowmelt, and nearby streams that run downslope towards the shared outlet, as well as the groundwater underneath the earth's surface. Drainage basins connect into other drainage basins at lower elevations in a hierarchical pattern, with smaller sub-drainage basins, which in turn drain into another common outlet.

Contents

The south bank of the Red River formed part of the US–Mexico border from the Adams–Onís Treaty (in force 1821) until the Texas Annexation and the Treaty of Guadalupe Hidalgo.

Adams–Onís Treaty treaty between the United States and Spain, ceding Florida to the U.S.

The Adams–Onís Treaty of 1819, also known as the Transcontinental Treaty, the Florida Purchase Treaty, or the Florida Treaty, was a treaty between the United States and Spain in 1819 that ceded Florida to the U.S. and defined the boundary between the U.S. and New Spain. It settled a standing border dispute between the two countries and was considered a triumph of American diplomacy. It came in the midst of increasing tensions related to Spain's territorial boundaries in North America against the United States and Great Britain in the aftermath of the American Revolution; it also came during the Latin American wars of independence.

Treaty of Guadalupe Hidalgo peace treaty that concludes Mexican-American War of 1846-1848

The Treaty of Guadalupe Hidalgo, officially titled the Treaty of Peace, Friendship, Limits and Settlement between the United States of America and the Mexican Republic, is the peace treaty signed on February 2, 1848, in the Villa de Guadalupe Hidalgo between the United States and Mexico that ended the Mexican–American War (1846–1848). The treaty came into force on July 4, 1848.

The Red River is the second-largest river basin in the southern Great Plains. [3] 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 1,360 miles (2,190 km), with a mean flow of over 57,000 cubic feet per second (1,600 m3/s) at the mouth.[ citation needed ]

Great Plains broad expanse of flat land west of the Mississippi River and east of the Rocky Mountains in the United States and Canada

The Great Plains is the broad expanse of flat land, much of it covered in prairie, steppe, and grassland, that lies west of the Mississippi River tallgrass prairie in the United States and east of the Rocky Mountains in the U.S. and Canada. It embraces:

Texas Panhandle Region in Texas, United States

The Texas Panhandle is a region of the U.S. state of Texas consisting of the northernmost 26 counties in the state. The panhandle is a rectangular area bordered by New Mexico to the west and Oklahoma to the north and east. The Handbook of Texas defines the southern border of Swisher County as the southern boundary of the Texas Panhandle region.

Oklahoma State of the United States of America

Oklahoma is a state in the South Central region of the United States, bordered by Kansas on the north, Missouri on the northeast, Arkansas on the east, Texas on the south, New Mexico on the west, and Colorado on the northwest. It is the 20th-most extensive and the 28th-most populous of the fifty United States. The state's name is derived from the Choctaw words okla and humma, meaning "red people". It is also known informally by its nickname, "The Sooner State", in reference to the non-Native settlers who staked their claims on land before the official opening date of lands in the western Oklahoma Territory or before the Indian Appropriations Act of 1889, which dramatically increased European-American settlement in the eastern Indian Territory. Oklahoma Territory and Indian Territory were merged into the State of Oklahoma when it became the 46th state to enter the union on November 16, 1907. Its residents are known as Oklahomans, and its capital and largest city is Oklahoma City.

Geography

Course

The Red River rises near the edge of the northwestern dip slope of the Llano Estacado mesa [4] in two forks in northern Texas and southwestern Oklahoma. The North Fork Red River meets the southern and largest fork near the Texas–Oklahoma border. The southern fork, which is about 120 miles (190 km) 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 (Not to be confused with another Palo Duro Creek 75 miles to the north which drains into the North Canadian River).

Dip slope topographic surface which slopes in the same direction as the dip of the underlying strata

A dip slope is a topographic (geomorphic) surface which slopes in the same direction, and often by the same amount, as the true dip or apparent dip of the underlying strata. A dip slope consists of the upper surface of a resistant layer of rock, often called caprock, that is commonly only slightly lowered and reduced in steepness by erosion. Dip slopes form the backslopes of cuestas, homoclinal ridges, hogbacks, and flatirons. The frontslopes of such ridges consist of either an escarpment, a steep slope, or perhaps even a line of cliffs. Generally, cuestas and homoclinal ridges are asymmetrical in that their dip slopes are less steep than their escarpments. In the case of hogbacks and flatirons, the dip of the rocks is so steep that their dip slope approaches the escarpment in their steepness.

Llano Estacado Southwestern United States in New Mexico and Texas

Llano Estacado, often translated as 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 (1.9 m/km).

North Fork Red River river in the United States of America

The North Fork Red River, sometimes called simply the "North Fork", is a tributary of the Red River about 271 mi (436 km) long, heading along the eastern Caprock Escarpment of the Llano Estacado about 11.4 mi (18.3 km) southwest of Pampa, Texas. Rising in Gray County, Texas, it terminates at the confluence with Prairie Dog Town Fork of the Red River at the Texas-Oklahoma border.

State Highway No. 78 Bridge at the Red River between Oklahoma and Texas, photographed on the Oklahoma side 78redriver.jpg
State Highway No. 78 Bridge at the Red River between Oklahoma and Texas, photographed on the Oklahoma side
Crossing the Red River at the Texas-Oklahoma border from I-35 HPIM2184.JPG
Crossing the Red River at the Texas–Oklahoma border from I-35
The Red River took a new channel near Natchitoches, Louisiana, and left behind Cane River Lake. Cane River Lake of the Red River, Natchitoches, LA IMG 1914.JPG
The Red River took a new channel near Natchitoches, Louisiana, 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 3,440 feet (1,050 m), [3] 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.

Palo Duro Canyon canyon system in the US state of Texas

Palo Duro Canyon is a canyon system of the Caprock Escarpment located in the Texas Panhandle near the cities of Amarillo and Canyon. As the second-largest canyon in the United States, it is roughly 120 mi (190 km) long and has an average width of 6 mi (9.7 km), but reaches a width of 20 mi (32 km) at places. Its depth is around 820 ft (250 m), but in some locations, it increases to 1,000 ft (300 m). Palo Duro Canyon has been named "The Grand Canyon of Texas" both for its size and for its dramatic geological features, including the multicolored layers of rock and steep mesa walls similar to those in the Grand Canyon.

Newlin is an unincorporated community in Hall County in the U.S. state of Texas.

Elmer, Oklahoma Town in Oklahoma, United States

Elmer is a town in Jackson County, Oklahoma, United States. The population was 96 at the 2010 census.

Point bars, abandoned meander loops, oxbow lakes in Lafayette and Miller counties, Arkansas RedRiverMeandersArkansas1.jpg
Point bars, abandoned meander loops, oxbow lakes 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.

Arkansas State of the United States of America

Arkansas is a state in the southern region of the United States, home to over 3 million people as of 2018. Its name is of Siouan derivation from the language of the Osage denoting their related kin, the Quapaw Indians. The state's diverse geography ranges from the mountainous regions of the Ozark and the Ouachita Mountains, which make up the U.S. Interior Highlands, to the densely forested land in the south known as the Arkansas Timberlands, to the eastern lowlands along the Mississippi River and the Arkansas Delta.

Muddy Boggy Creek, also known as the Muddy Boggy River, is a 175-mile-long (282 km) river in south central Oklahoma. The stream headwaters arise just east of Ada in Pontotoc County. It is a major tributary of the Red River in south central Oklahoma. Clear Boggy Creek is a major tributary which enters the Muddy Boggy at a location known as River Mile 24 in Choctaw County. The river is inhabited by over one hundred species of fish.

Texarkana, Arkansas City in the United States

Texarkana is a city in Arkansas and the county seat of Miller County. The city is located across the state line from its twin city, Texarkana, Texas. The city was founded at a railroad intersection on December 8, 1873, and was incorporated in Arkansas on August 10, 1880. Texarkana is the principal city of the Texarkana metropolitan area, which is ranked 274th in terms of population in the United States with 150,098 in 2016 according to the United States Census Bureau.

Soon after, the river 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 [5] 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. [6]

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, Little Wichita River, Little River, Sulphur River, Loggy Bayou (through Lake Bistineau and Dorcheat Bayou) as well as the Ouachita River (also known as the Black River at that point) not far (at Acme, Louisiana) from the mouth.

Saltwater river

Salt beds in the Red River Little Red River Texas 2015.jpg
Salt beds in the Red 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. The problem with the water in the Red River is much of it is too salty and requires costly treatment, if it is usable at all. [7] [8]

Watershed

The Red River's watershed covers 65,590 square miles (169,900 km2) [3] 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. [3] By the time of European contact, the eastern Piney Woods were dominated by the numerous historic tribes of the Caddoan Confederacy. They found plentiful game and fish, and also had good land for cultivating staple crops. [3] 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. [3] 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. [3]

European-American exploration and settlement

Crossing the Red River near Granite, Oklahoma, 1921. Theb0771 - Flickr - NOAA Photo Library.jpg
Crossing the Red River near Granite, Oklahoma, 1921.

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. [9] 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. [10] 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. [11]

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 [11] 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 (March–May 1864) 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

Red River, Texas Red River Texas.jpg
Red River, Texas

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 160 miles (260 km) 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. [5]

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.

Greer County debate

Specialists debate whether the North Fork or the Prairie Dog Town Fork is the true stem. [3] Because of a cartographic error, the land between the north and south forks was claimed by both the state of Texas and the United States federal government. Randolph B. Marcy's expedition followed the Prairie Dog Town Fork in 1852. [3] Originally called Greer County, Texas, the US Supreme Court ruled that it belonged to the United States, which at the time oversaw the Oklahoma Territory. That territory was later incorporated into the state of Oklahoma, whose southern border now follows the south fork. Today, the southern Prairie Dog Town Fork is considered the main fork, though the North Fork is as long and normally has a greater water flow. [3]

2015 Red River flood

In June 2015, the Red River flooded parts of northeast Texas, southwest Arkansas, southeast Oklahoma and Louisiana, from Denison Dam, to just south of Alexandria, Louisiana. [12]

Recreation

Red River LA 2 Bridge, not the Jimmie Davis Bridge, atop the Red River between Bossier and Caddo parishes near Shreveport Revised bridge atop Red River in LA IMG 6337.jpg
Red River LA 2 Bridge, not the Jimmie Davis Bridge, atop the Red River between Bossier and Caddo parishes near Shreveport
Popular pedestrian walkway along the Red River in Alexandria, Louisiana Pedestrian walkway at Red River, Alexandria, LA IMG 4300.JPG
Popular pedestrian walkway along the Red River in Alexandria, Louisiana

In 1943, Denison Dam was built on the Red River to form Lake Texoma, a large reservoir of 89,000 acres (360 km2), some 70 miles (110 km) north of Dallas. Other reservoirs on the river's tributaries serve as flood control.

See also

Related Research Articles

Sabine River (Texas–Louisiana) river in the United States of America

The Sabine River is a river, 510 miles (820 km) long, in the Southern U.S. states of Texas and Louisiana. In its lower course, it forms part of the boundary between the two states and empties into Sabine Lake, an estuary of the Gulf of Mexico. Over the first half of the 19th century, the river formed part of the Spanish–American, Mexican–American, and Texan–American international boundaries. The upper reaches of the river flow through the prairie country of northeast Texas. Along much of its lower reaches, it flows through the pine forests along the Texas–Louisiana border, and the bayou country near the Gulf Coast.

Arkansas River major tributary of the Mississippi River, United States

The Arkansas River is a major tributary of the Mississippi River. It generally flows to the east and southeast as it traverses the U.S. states of Colorado, Kansas, Oklahoma, and Arkansas. The river's source basin lies in the western United States in Colorado, specifically the Arkansas River Valley, where the headwaters derive from the snowpack in the Sawatch and Mosquito mountain ranges. It then flows east into the Midwest via Kansas, and finally into the South through Oklahoma and Arkansas.

Ouachita River river in the United States of America

The Ouachita River is a 605-mile-long (974 km) river that runs south and east through the U.S. states of Arkansas and Louisiana, joining the Tensas River to form the Black River near Jonesville, Louisiana. It is the 25th-longest river in the United States.

The Jefferson Highway was an automobile highway stretching through the central United States from New Orleans, Louisiana, to Winnipeg, Manitoba, Canada. The Jefferson Highway was replaced with the new numbered US Highway system in the late 1920s. Portions of the highway are still named Jefferson Highway, for example: the portions that run through Jefferson Parish, Louisiana; East Baton Rouge Parish, Louisiana; Lee's Summit, Missouri; Osseo, Minnesota; and Wadena, Minnesota.

The Great Raft was a gigantic log jam or series of "rafts" that clogged the Red and Atchafalaya Rivers and was unique in North America in terms of its scale.

U.S. Route 71 highway in the United States

U.S. Route 71 is a major north–south United States highway that extends for over 1500 miles in the central United States. This original 1926 route has remained largely unchanged by encroaching Interstate highways. Currently, the highway's northern terminus is in International Falls, Minnesota at the Canada–US border, at the southern end of the Fort Frances-International Falls International Bridge to Fort Frances, Ontario. U.S. Route 53 also ends here. On the other side of the bridge, Trans-Canada Highway 11 is an east–west route. US 71's southern terminus is between Port Barre and Krotz Springs, Louisiana at an intersection with U.S. Route 190.

Atchafalaya River river in the United States of America

The Atchafalaya River is a 137-mile-long (220 km) distributary of the Mississippi River and Red River in south central Louisiana in the United States. It flows south, just west of the Mississippi River, and is the fifth largest river in North America, by discharge. The name "Atchafalaya" comes from Choctaw for "long river", from hachcha, "river", and falaya, "long".

Canadian River river in Texas and Oklahoma

The Canadian River is the longest tributary of the Arkansas River in the United States. It is about 906 miles (1,458 km) long, starting in Colorado and traveling through New Mexico, the Texas Panhandle, and Oklahoma. The drainage area is about 47,700 square miles (124,000 km2).

Lake Texoma reservoir on the border of the U.S. states of Texas and Oklahoma

Lake Texoma is one of the largest reservoirs in the United States, the 12th largest US Army Corps of Engineers' (USACE) lake, and the largest in USACE Tulsa District. Lake Texoma is formed by Denison Dam on the Red River in Bryan County, Oklahoma, and Grayson County, Texas, about 726 miles (1,168 km) upstream from the mouth of the river. It is located at the confluence of the Red and Washita Rivers. The project was completed in 1944. The damsite is about 5 miles (8.0 km) northwest of Denison, Texas, and 15 miles (24 km) southwest of Durant, Oklahoma. Lake Texoma is the most developed and most popular lake within the USACE Tulsa District, attracting around 6 million visitors a year. Oklahoma has more of the lake within its boundaries than Texas.

Greer County, Texas County in the United States

Greer County, a county created by the Texas legislature on February 8, 1860, was land claimed by both Texas and the United States.

Texoma Region

Texoma is an interstate region in the United States, split between Oklahoma and Texas. The name is a portmanteau of Texas and Oklahoma. Like many regional names, businesses use the term Texoma in their name to describe their intended service area.

Salt Fork Red River river in the United States of America

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 Prairie Dog Town Fork Red River about 21 km (13 mi) south of Altus of Jackson County, Oklahoma.

Prairie Dog Town Fork Red River river in the United States of America

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.

Little Red River (Texas) river in United States of America

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.

References

  1. Caddo name. Meredith, Howard. "Caddo (Kadohadacho)." Archived 2010-07-19 at the Wayback Machine Oklahoma Historical Society's Encyclopedia of Oklahoma History and Culture. Retrieved 9 Sept 2012)
  2. Tyson, Carl N. The Red River in Southwestern History. Norman: University of Oklahoma Press, 1981. ISBN   0-8061-1659-5
  3. 1 2 3 4 5 6 7 8 9 10 Benke, Arthur; Colbert Cushing (2005). River of North America. Academic Press. p. 1144. ISBN   9780120882533.
  4. John Miller Morris, El Llano Estacado: Exploration and Imagination on the High Plains, 2003.
  5. 1 2 Piazza, Bryan P (2014). The Atchafalaya River Basin: History and Ecology of an American Wetland. Texas A&M University Press. ISBN   978-1-62349-039-3.
  6. Frederick Marcel Spletstoser (2005). Talk of the Town: The Rise of Alexandria, Louisiana, and the Daily Town Talk. Baton Rouge, Louisiana: Louisiana State University Press. pp. 125–126. ISBN   0-8071-2934-8 . Retrieved July 24, 2015.
  7. https://www.texastribune.org/2013/11/21/along-salty-red-river-communities-seek-feds-help/ . Retrieved 25 December 2018.
  8. https://pubs.usgs.gov/fs/fs-170-97/FS_170-97.htm . Retrieved 25 December 2018.
  9. Jefferson to Dunbar, 25 May 1805, quoted in T. Lindsay Baker, ed., The Texas Red River country: the official surveys of the headwaters, 1876, 1998: "Foreword", v, and in D.L. Flores, "The Ecology of the Red River in 1806: Peter Custis and Early " The Southwestern Historical Quarterly 88,.1, (July 1984).
  10. R.B. Marcy, Exploration of the Red River of Louisiana: in the year 1852... with Reports on the Natural History of the Country, Washington, 1853.
  11. 1 2 Harbour, Emma Estill. "A Brief History of the Red River County since 1803. Chronicles of Oklahoma. Vol. 16. No. 1. March 1938. Retrieved September 7, 2013.
  12. http://www.msn.com/en-us/weather/topstories/with-homes-underwater-in-louisiana-recovery-teams-head-out/ar-BBkYtRO?ocid=mailsignout
  13. "Bridgehunter.com | Red River of the South". bridgehunter.com. Retrieved 2017-01-07.
Geology