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Ohio River

 
Dictionary: Ohio River


A river formed by the confluence of the Allegheny and Monongahela rivers in western Pennsylvania and flowing about 1,578 km (981 mi) to the Mississippi River at Cairo in southern Illinois. Control of the river was contested by the British and French until 1763. The region was ceded to the United States at the end of the Revolutionary War (1783).

 

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Major river, eastern central U.S. Formed by the confluence of the Allegheny and Monongahela rivers, it flows northwest out of Pennsylvania, and west and southwest to form the state boundaries of Ohio – West Virginia, Ohio-Kentucky, Indiana-Kentucky, and Illinois-Kentucky. After a course of 975 mi (1,569 km), it empties into the Mississippi River at Cairo, Ill. It is navigable and has supported commerce since the earliest settlements. The river's strategic importance was recognized by the 1750s. After the French and Indian War, the English controlled the territory around the river.

For more information on Ohio River, visit Britannica.com.

US History Encyclopedia: Ohio River
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Ohio River, the major eastern tributary of the Mississippi River, is also a significant river artery in the north central United States, extending for 981 miles from Pittsburgh, Pennsylvania, to Cairo, Illinois. Formed by the confluence of the Allegheny and Monongahela rivers (325 and almost 130 miles in length, respectively), at the Forks of the Ohio, the river flows northwest from the Keystone State before turning southwest and joining the Mississippi River at Cairo. At Pittsburgh the Ohio is 1,021 feet above sea level, and 322 feet at Cairo. The Falls of the Ohio at Louisville, Kentucky, is a 2.2-mile-long limestone rapids where the river drops 23.9 feet. Canalization around the rapids was completed in 1830, ensuring navigability. Between Pittsburgh and Wheeling, West

Virginia, the river averages 0.5 miles in width; between Cincinnati, Ohio, and Louisville, 1.1 miles; and from Louisville to Cairo, 1.3 miles.

The Ohio River and its valley have a complex geological history but are young, formed at the end of the Pleistocene epoch, about ten thousand years ago. The valley is narrow and characterized by steep bluffs, and the drainage basin includes about 203,900 square miles and has an annual average flow of 281,000 cubic feet per second. Six major tributaries join the Ohio from the north: the Wabash (Illinois-Indiana border); Muskingum, Miami, Hocking, and Scioto (Ohio); and Beaver (Pennsylvania). From the south the major tributaries are the Great Kanawha and Guyandotte (West Virginia); Big Sandy (West Virginia–Kentucky border); and Licking, Kentucky, Salt, Green, Cumberland, and Tennessee (Kentucky). About 80 percent of the state of Ohio and 85 percent of Kentucky drain into the Ohio-Mississippi system, and there are over 2,900 miles of navigable rivers in the ten-state area of the Ohio River system.

Politically the Ohio River marks the boundaries of five states: Ohio and West Virginia, Ohio and Kentucky, Indiana and Kentucky, and Illinois and Kentucky. In addition to Pittsburgh, the banks of the Ohio serve as the site of five major cities in Ohio (Cincinnati, Gallipolis, Marietta, Portsmouth, and Steubenville); four in Indiana (Madison, New Albany, Evansville, and Mount Vernon); three in West Virginia (Parkersburg, Huntington, and Wheeling); and five in Kentucky (Ashland, Covington, Louisville, Owensboro, and Paducah).

Bibliography

Banta, Richard E. The Ohio. Rivers of America Series 39. New York: Rinehart, 1949; reprinted Lexington: University Press of Kentucky, 1998.

Klein, Benjamin F., and Eleanor Klein, eds. The Ohio River Handbook and Picture Album. Cincinnati: Young and Klein, 1969.

 
Ohio, river, 981 mi (1,579 km) long, formed by the confluence of the Allegheny and Monongahela rivers in SW Pa., at Pittsburgh; it flows northwest, then generally southwest to enter the Mississippi River at Cairo, Ill. The Ohio's course follows a portion of the southern edge of the region covered by continental ice during the late Cenozoic era; glacial meltwater probably cut its original channel. The river is a major tributary of the Mississippi and supplies more water to it than does the Missouri River. The Ohio River basin covers c.204,000 sq mi (528,400 sq km); the chief tributaries are the Tennessee, Cumberland, Wabash, and Kentucky.

Flood Control and Canals

The Ohio is prone to spring flooding, and extensive flood control and protection devices have been constructed along the river and its tributaries. These devices also improve the river's navigability; a 9-ft (2.7-m) channel is maintained along its entire length. A system of modern locks and dams, constructed since 1955 to replace older structures, speeds the transit of barges and leisure craft. A canal (first opened in 1830) at Louisville bypasses the Falls of the Ohio, a 21/4-mi (3.6-km)-long series of rapids having a 24-ft (7-m) drop.

Human Impact

The Ohio River basin is one of the most populated and industrialized regions of the United States. Oil and steel account for most of the cargoes moved on the river. The principal river ports are Cincinnati, Louisville, and Pittsburgh. Eight states (Ill., Ind., Ky., N.Y., Ohio, Pa., Va., and W.Va.) affected by the river's industrial pollution ratified (1948) the Ohio River Valley Sanitation Compact. Some results of their cleanup efforts have become discernible, and the river now supports marinas and recreational facilities.

History

The French explorer La Salle reportedly reached the Ohio River in 1669, but there was no significant interest in the valley until the French and the British began to struggle for control of the river in the 1750s. An early settlement was established at the forks of the Ohio (modern Pittsburgh) by the Ohio Company of Virginia in 1749, but it was captured by the French in 1754, and the unfinished Fort Prince George was renamed Fort Duquesne; it was recaptured by the British and renamed Fort Pitt in 1758. At the end of the French and Indian Wars, Britain gained control of the river by the treaty of 1763, but settlement of the area was prohibited. Britain ceded the region to the United States at the end of the Revolutionary War (1783), and it was opened to settlement by the Ordinance of 1787, which established the Northwest Territory.

Until the opening of the Erie Canal in 1825, the Ohio River was the main route to the newly opened West and the principal means of market transportation of the region's growing farm output. Traffic declined on the river after the railroads were built in the mid-1800s, although it revived after World War II. Comparatively little traffic remains on the Ohio, despite the new locks, dams, and channel improvements, which were all meant to spur economic activity on the river.

Bibliography

See W. Havighurst, River to the West (1970); W. Burmeister, Appalachian Waters 5: The Upper Ohio and Its Tributaries (1978).


Geography: Ohio River
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River that runs west from Pittsburgh to the Mississippi River.

Wikipedia: Ohio River
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Ohio River (Oyo)
River
The widest point on the Ohio River is just west of downtown Louisville, where it is one-mile wide
Country United States
States Pennsylvania, Ohio, West Virginia, Kentucky, Indiana, Illinois
Tributaries
 - left Kanawha River, Big Sandy River, Kentucky River, Cumberland River, Tennessee River, Licking River
 - right Beaver River, Muskingum River, Scioto River, Great Miami River, Wabash River
Cities Pittsburgh, PA, Cincinnati, OH, Louisville, KY, Owensboro, KY, Evansville, IN, Huntington, WV, Paducah, KY, Cairo, IL
Source Allegheny River
 - location Allegany Township, Pennsylvania
 - elevation 2,240 ft (683 m)
 - coordinates 41°51′24″N 77°52′30″W / 41.85667°N 77.875°W / 41.85667; -77.875
Secondary source Monongahela River
 - location Fairmont, West Virginia
 - elevation 880 ft (268 m)
 - coordinates 39°27′53″N 80°09′13″W / 39.46472°N 80.15361°W / 39.46472; -80.15361
Source confluence
 - location Pittsburgh, Pennsylvania
 - elevation 730 ft (223 m)
 - coordinates 40°26′32″N 80°00′52″W / 40.44222°N 80.01444°W / 40.44222; -80.01444
Mouth Mississippi River
 - location Cairo, Illinois
 - elevation 290 ft (88 m)
 - coordinates 36°59′12″N 89°07′52″W / 36.98667°N 89.13111°W / 36.98667; -89.13111
Length 981 mi (1,579 km)
Basin 189,422 sq mi (490,601 km2)
Discharge for Cairo, IL
 - average 281,000 cu ft/s (7,957 m3/s)
Ohio River basin
The Allegheny river (left) and Monongahela river (right) join to form the Ohio River at Pittsburgh, Pennsylvania, the largest metropolitan area on the river.
Cincinnati, Ohio is a well-known city along the Ohio River, historically known for its riverboats. The Tall Stacks festival celebrates the Cincinnatti riverboats and the Ohio River every three or four years.
Louisville, Kentucky, the largest city on the river, is situated at both the widest and deepest level of the Ohio River.
Evansville, Indiana, the third-largest city in Indiana and the fourth-largest city on the river
A barge hauling coal in the Louisville and Portland Canal, the only man-made portion of the Ohio River

The Ohio River is the largest tributary, by volume, of the Mississippi River. It is approximately 981 miles (1,579 km) long and is located in the eastern United States.

The river had great significance in the history of the Native Americans, as numerous civilizations formed along its valley. In the last five centuries prior to European contact, the Mississippian culture built numerous regional chiefdoms and major earthwork mounds in the Ohio Valley, such as Angel Mounds near Evansville, Indiana. For thousands of years, Native Americans, like the European explorers and settlers who followed them, used the river as a major transportation and trading route. About 1200 CE, the area of Kentucky was the site of longterm wars between the Iroquois, invading from present-day New York, and the Osage and other Ohio River tribes. Over centuries, the Osage, Omaha, Ponca and Kaw migrated west of the Mississippi River, settling by the mid-17th century in their historic grounds in Missouri, Arkansas, and Oklahoma, and nearby states.

After European-American settlement, the river served at times as a border between present-day Kentucky and Indian Territories. It was a primary transportation route during the westward expansion of the early U.S. The Ohio flows through or along the border of six states, and its drainage basin encompasses 14 states. Through its largest tributary, the Tennessee River, the basin includes many of the states of the southeastern U.S.

During the nineteenth century, the river was the southern boundary of the Northwest Territory, thus serving as the border between free and slave territory. It is sometimes referred to as the "Mason-Dixon line". It is commonly acknowledged as the western natural extension of the original Mason-Dixon line that divided Pennsylvania and Delaware from Maryland and West Virginia (then a part of Virginia.) It was thus the unofficial and, at times disputed, border between the Northern United States and the American South or Upper South.

The Ohio River is a climatic transition area, as its water runs along the periphery of the humid subtropical climate and humid continental climate. It is inhabited by fauna and flora of both climates. In his Notes on the State of Virginia published in 1781-82, Thomas Jefferson stated: "The Ohio is the most beautiful river on earth. Its current gentle, waters clear, and bosom smooth and unbroken by rocks and rapids, a single instance only excepted."[1]

Contents

Geography and hydrography

The river is formed by the confluence of the Allegheny and Monongahela rivers. Point State Park in Pittsburgh, Pennsylvania marks the confluence. From Pittsburgh, it flows northwest through Allegheny and Beaver Counties, before making an abrupt turn to the south-southwest at the West Virginia—OhioPennsylvania triple-state line (near East Liverpool, Ohio, Chester, West Virginia, and Midland, Pennsylvania). From there, it forms the border between West Virginia and Ohio, upstream of Wheeling, West Virginia.

The river then follows a roughly southwest and then west-northwest course until Cincinnati, before bending to a west-southwest course for most of its length. It flows along the borders of West Virginia, Ohio, Kentucky, Indiana, and Illinois, until it joins the Mississippi near the city of Cairo, Illinois.

Major tributaries of the river, indicated by the location of the mouths, include:

Drainage basin

The Ohio's drainage basin covers 189,422 square miles (490,603 km²), including the easternmost regions of the Mississippi Basin. States drained by the Ohio include:

Geology

From a geologic standpoint, the Ohio River is young. The river formed on a piecemeal basis beginning between 2.5 and 3 million years ago. The earliest Ice Ages occurred at this time and dammed portions of north-flowing rivers. The Teays River was the largest of these rivers. The modern Ohio River flows within segments of the ancient Teays. The ancient rivers were rearranged or consumed by glaciers and lakes.

Upper Ohio River

The upper Ohio River formed when one of the glacial lakes overflowed into a south-flowing tributary of the Teays River. Prior to that event, the north-flowing Steubenville River (no longer in existence) ended between New Martinsville and Paden City, West Virginia. Likewise, the south-flowing Marietta River (no longer in existence) ended between the present-day cities. The overflowing lake carved through the separating hill and connected the rivers.

The resulting floodwaters enlarged the small Marietta valley to a size more typical of a large river. The new large river subsequently drained glacial lakes and melting glaciers at the end of several Ice Ages. The valley grew with each major Ice Age.

Many small rivers were altered or abandoned after the upper Ohio River formed. Valleys of some abandoned rivers can still be seen on satellite and aerial images of the hills of Ohio and West Virginia between Marietta, Ohio, and Huntington, West Virginia. As testimony to the major changes that occurred, such valleys are found on hilltops.[clarification needed]

Middle Ohio River

The middle Ohio River formed in a manner similar to formation of the upper Ohio River. A north-flowing river was temporarily dammed southwest of present-day Louisville, Kentucky, creating a large lake until the dam burst. A new route was carved to the Mississippi River. Eventually the upper and middle sections combined to form what is essentially the modern Ohio River.

History

Confluence of the Mississippi and Ohio Rivers at Cairo, Illinois.
Carl D. Perkins Bridge in Portsmouth, Ohio with Ohio River and Scioto River tributary on right.
Silver Bridge in Point Pleasant, West Virginia which collapsed into the Ohio River in 1967, and gained notoriety through John Keel's 1976 book and subsequent 2002 movie The Mothman Prophecies.

Since it was considered by pre-Columbian inhabitants of eastern North America to be part of a single river continuing on through the lower Mississippi, it is perhaps an understatement to characterize the Ohio as a tributary of the Mississippi River.[citation needed] The river is 981 miles (1,579 km) long and carries the largest volume of water of any tributary of the Mississippi. The Indians and early explorers and settlers of the region often considered the Allegheny to be part of the Ohio. The forks (the confluence of the Allegheny and Monongahela rivers at what is now Pittsburgh) was considered a strategic military location.

In 1669 René-Robert Cavelier, Sieur de La Salle, led an expedition of French traders who became the first Europeans to see the river. He traveled from Canada and entered the headwaters of the Ohio, traveling as far as the Falls of Ohio before turning back. He returned to explore the river again in other expeditions. An Italian cartographer traveling with him created the first map of the Ohio River. France claimed ownership of the river until its territory in North America was ceded to Great Britain in 1763, following the Seven Years War (aka the French and Indian War.)

On May 19, 1749, King George II of Great Britain granted the Ohio Company a charter of land around the forks. Exploration of the territory and trade with the Indians in the region near the Forks by British colonials from Pennsylvania and Virginia—both of which claimed the territory—led to conflict with French forces that also claimed the region and had built forts along the Allegheny River. This directly led to the French and Indian War in North America. The French and Indian War was part of a more global conflict, the Seven Years' War between England and France. After several initial defeats, the British eventually gained sovereignty over the Ohio Valley.

The 1768 Treaty of Fort Stanwix opened Kentucky to colonial settlement and established the Ohio River as a southern boundary for American Indian territory.[2] In 1774, the Quebec Act restored the land east of the Mississippi River and north of the Ohio River to Quebec, appeasing the French-speaking British subjects, but angering the Thirteen Colonies. They listed it as one of the Intolerable Acts which precipitated the American Revolution.

Louisville, Kentucky was founded at the only major natural navigational barrier on the river, the Falls of the Ohio. The Falls were a series of rapids where the river dropped 26 feet (7.9 m) in a stretch of about 2 miles (3.2 km). In this area, the river flowed over hard, fossil-rich beds of limestone. The first locks on the river were built in 1825 at Louisville to circumnavigate the falls. Today it is the site of McAlpine Locks and Dam.

Because the Ohio River flowed westwardly, it became a convenient means of westward movement by pioneers traveling from western Pennsylvania. After reaching the mouth of the Ohio, settlers would travel north on the Mississippi River to St. Louis, Missouri. There, some continued on up the Missouri River, some up the Mississippi, and some further west over land routes. In the early 19th century, pirates such as Samuel Mason, settled at Cave-In-Rock, Illinois, waylaid travelers on their way down the river. They killed travelers, stealing their goods and scuttling their boats. The folktales about Mike Fink recall the keelboats used for commerce in the early days of European settlement. The Ohio River boatmen were the inspiration for performer Dan Emmett, who in 1843 wrote the song "The Boatman's Dance".

Trading boats and ships traveled south on the Mississippi to New Orleans, and sometimes beyond to the Gulf of Mexico and other ports in the Americas and Europe. This provided a much-needed export route for goods from the west, since the trek east over the Appalachian Mountains was long and arduous. The need for access to the port of New Orleans by settlers in the Ohio Valley led to the Louisiana Purchase in 1803.

Because the river is the southern border of Ohio, Indiana and Illinois, it was part of the border between free tates and slave states in the years before the American Civil War. The expression "sold down the river" originated as a lament of Upper South slaves, especially from Kentucky, who were separated from their families and sold in Louisville and other Kentucky locations to be shipped via the Ohio River and Mississippi down to New Orleans. There they were sold to owners of cotton and sugar field plantations in the Deep South, which were notoriously hard on laborers.[3][4] Before and during the Civil War, the Ohio River was called the "River Jordan" by slaves' crossing it to escape to freedom in the North via the Underground Railroad.[5] Such escapes were depicted in contemporary anti-slavery novels, such as Harriet Beecher Stowe's Uncle Tom's Cabin. The times have also been portrayed by late 20th century novelists such as Toni Morrison. More escaping slaves made their perilous journey north to freedom across the Ohio River than anywhere else across the north-south frontier.

Today, the Ohio River is considered to separate Midwestern Great Lakes states from Southern states which were historically border states in the Civil War.

Mouth of the Ohio, as it feeds into the Mississippi

The charter for Virginia went to the far shore of the Ohio River, so that the entire river was included in the lands "owned" by Virginia. Where the river serves as a boundary between states today, the entire river belongs to the states on the east and south, i.e., West Virginia and Kentucky, that were divided from Virginia. Thus Wheeling Island, the largest inhabited island in the Ohio River, belongs to West Virginia, even though it is closer to the Ohio shore than to the West Virginia shore. Kentucky brought suit against Indiana in the early 1980s because of the building of the Marble Hill nuclear power plant in Indiana, which would have discharged its waste water into the river.

The U.S. Supreme Court held that Kentucky's jurisdiction (and, implicitly, that of West Virginia) extended only to the low-water mark of 1793 (important because the river has been extensively dammed for navigation, so that the present river bank is north of the old low-water mark.) Similarly, in the 1990s, Kentucky challenged Illinois' right to collect taxes on a riverboat casino docked in Metropolis, citing its own control of the entire river. A private casino riverboat that docked in Evansville, Indiana on the Ohio River opened about the same time. Although such boats cruised on the Ohio River in an oval pattern up and down, the state of Kentucky soon protested. Other states had to limit their cruises to going forwards then reversing and going backwards on the Indiana shore only.

In the early 1980s, the Falls of the Ohio National Wildlife Conservation Area was established at Clarksville, Indiana.

River depth

Lawrenceburg, Indiana, is one of many towns that use the Ohio as a shipping avenue.

The Ohio River is a naturally shallow river that was artificially deepened by series of dams. The dams raise the water level and have turned the river largely into a series of reservoirs, eliminating shallow stretches and allowing for commercial navigation. Near its origin at the confluence of the Allegheny and Monongahela Rivers, the Ohio remains fairly shallow, never rising above around 30 feet (9 m) deep all the way past Cincinnati. From its origin to Cincinnati, the average depth is approximately 27 feet (8 m). However, once past Cincinnati, the river deepens substantially. Due to the damming, along with glacier formations and migrations in the latter part of the second Ice Age, the river's depth increases nearly fivefold over about 100 miles (161 km), coming to a maximum depth of 168 feet (51 m) just west of Louisville, Kentucky. The 50 miles (80 km) around Louisville represent the deepest area of the river with an average depth of approximately 132 feet (40 m), allowing for much larger vessels to traverse the river. From Louisville, the river loses its depth very gradually until its confluence with the Mississippi at Cairo, Illinois, where it has an approximate depth of 20 feet (6 m), because it is more free flowing. The natural depth of the river varies from about 3 feet to 40 feet.

Water levels for the Ohio River are predicted daily by the National Oceanic and Atmospheric Administration's Ohio River Forecast Center. The water depth predictions are relative to each local flood plain based upon predicted rainfall in the Ohio River basin in five reports as follows:

Panorama of the Ohio at its widest point, just west of downtown Louisville, Kentucky

Cities and towns along the river

Metro Area Population
Pittsburgh 2.3 million
Cincinnati 2.2 million
Louisville 1.2 million
Evansville 350,000
Huntington 290,000
Parkersburg 160,000
Wheeling 145,000
Weirton-Steubenville 132,008
Owensboro 112,000

Cities along the Ohio include:

Recreation

The world record for the largest blue catfish 104 pounds (47.2 kilograms) taken in the line class was set on the Ohio River in 1999. The river also holds records for the following species for the state of Kentucky:[7]

  • Saugeye, 6.58 pounds (3 kilograms)

The Ohio River from Cairo, Illinois to Smithland, Kentucky comprises a significant portion of the Great Loop, the circumnavigation of Eastern North America by water for recreational purposes.[citation needed]

References

  1. ^ Jefferson, Thomas, 1743-1826. Notes on the State of Virginia
  2. ^ *Taylor, Alan (2006). The Divided Ground: Indians, Settlers, and the Northern Borderland of the American Revolution. New York: Alfred A. Knopf. p. 44, see map on 39. ISBN 0-679-45471-3. 
  3. ^ KET's Underground Railroad - Behind the Scenes - Guy Mendes
  4. ^ "Put in Master's Pocket: Interstate Slave Trading and the Black Appalachian Diaspora"
  5. ^ KET's Underground Railroad - Community Research
  6. ^ River Watch - Ohio River Basin
  7. ^ "Kentucky State Record Fish List". Kentucky Department of Fish and Wildlife Resources. 2006-04-17. http://fw.ky.gov/recordfish.asp. Retrieved 2007-02-17. 

See also

External links


 
 

 

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Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2007. Published by Houghton Mifflin Company. All rights reserved.  Read more
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Columbia Encyclopedia. The Columbia Electronic Encyclopedia, Sixth Edition Copyright © 2003, Columbia University Press. Licensed from Columbia University Press. All rights reserved. www.cc.columbia.edu/cu/cup/ Read more
Geography. The New Dictionary of Cultural Literacy, Third Edition Edited by E.D. Hirsch, Jr., Joseph F. Kett, and James Trefil. Copyright © 2002 by Houghton Mifflin Company. Published by Houghton Mifflin. All rights reserved.  Read more
Wikipedia. This article is licensed under the Creative Commons Attribution/Share-Alike License. It uses material from the Wikipedia article "Ohio River" Read more