| Ohio River (Oyo) |
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 |
| Major cities |
Pittsburgh, PA, Cincinnati, OH,
Louisville, KY, Evansville, IN |
| Length |
mi ( km) |
| Watershed |
mi² ( km²) |
| Discharge at |
Cairo, IL |
| - average |
ft³/s
( m³/s)
(1951-80) [1] |
| Primary source |
Allegheny River |
| - location |
Allegany Township, Pennsylvania |
| - coordinates |
41°51′24″N 77°52′30″W / 41.85667,
-77.875 |
| - elevation |
ft ( m) |
| - length |
mi ( km) |
| Other source |
Monongahela River |
| - location |
Fairmont, West Virginia |
| - coordinates |
39°27′53″N 80°09′13″W / 39.46472,
-80.15361 |
| - elevation |
ft ( m) |
| - length |
mi ( km) |
| Source
confluence |
| - location |
Pittsburgh, Pennsylvania |
| - coordinates |
40°26′32″N 80°00′52″W / 40.44222,
-80.01444 |
| - elevation |
ft ( m) |
| Mouth |
Mississippi River |
| - location |
Cairo, Illinois |
| - coordinates |
36°59′12″N 89°07′52″W / 36.98667,
-89.13111 |
| - elevation |
ft ( m) |
| Major
tributaries |
| - left |
Kanawha River, Kentucky River,
Cumberland River, Tennessee River |
| - right |
Wabash River |
|
|
Cincinnati, Ohio is a well known city along the Ohio River, historically known for its
riverboats. The
Tall Stacks festival annually celebrates
this connection between Cincinnati and 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. It was a primary
transportation route during the westward expansion of the early U.S. It flows through or along the border of six states, and its watershed encompasses 14 states, including many of
the states of the southeastern U.S. through its largest tributary, the
Tennessee River. During the eighteenth century, it 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" as it is commonly acknowledged as the western natural extension of the original
Mason-Dixon line that divided Pennsylvania, Maryland, Delaware, and West Virginia (and at one time part of Virginia) thus being
the unofficial, and at times disputed, border between the Northern United States
and the American South or upland South. The
Ohio River interestingly is also a climatic transition area, its water runs along the periphery of the humid subtropical climate and humid
continental climate thereby being inhabited by fauna and flora of both climates.
Geography and hydrography
The river is formed by the confluence of the Allegheny and Monongahela rivers at Point State Park in Pittsburgh, Pennsylvania. From Pittsburgh, it flows northwest through Allegheny & Beaver Counties,
before making an abrupt turn to the south-southwest at the West Virginia—Ohio—Pennsylvania triple state line (near East Liverpool, Ohio, Chester, West Virginia, and
Midland, Pennsylvania), from which point 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 before bending to a west-southwest course for most
of its length. It flows along the borders of West Virginia, Kentucky, Ohio, Indiana, and
Illinois, until it joins the Mississippi near the
city of Cairo, Illinois.
Major tributaries of the river, indicated by the location of their mouth, include:
- Allegheny River — Pittsburgh,
Pennsylvania
- Monongahela River — Pittsburgh,
Pennsylvania
- Chartiers Creek - Pittsburgh,
Pennsylvania
- Beaver River — Rochester,
Pennsylvania
- Wheeling Creek — Wheeling, West Virginia
- Little Muskingum River — Ohio
- Duck Creek — Ohio
- Muskingum River — Marietta, Ohio
- Little Kanawha River — Parkersburg, West Virginia
- Hocking River — Ohio
- Kanawha River — Point Pleasant, West Virginia
- Guyandotte River — Huntington, West Virginia
- Big Sandy River — Kentucky-West Virginia border
- Scioto River — Portsmouth, Ohio
- Little Miami River — Cincinnati, Ohio
- Licking River — Newport-Covinton, Kentucky
- Great Miami River — Ohio-Indiana border
- Salt River — West Point,
Kentucky
- Kentucky River — Carrollton, Kentucky
- Green River — Kentucky
- Wabash River — Indiana-Illinois border
- Saline River — Illinois
- Cumberland River — Kentucky
- Tennessee River — Paducah, Kentucky
- Cache River — Illinois
Drainage basin
The Ohio's drainage basin covers 189,422 square miles (490,603 km²), including the eastern-most regions of the
Mississippi Basin. States drained by the Ohio include:
- Illinois (the southeast quarter of the state),
- Indiana (all but the northern area of the state),
- Ohio (the southern half of the state),
- New York (a small area of the southern border along the headwaters of the Allegheny River),
- Pennsylvania (a corridor from the southwestern corner to north central border),
- Maryland (a small corridor along the Youghiogheny
River on the state's western border),
- West Virginia (all but the eastern panhandle of the state),
- Kentucky (all but a small part in the extreme
west of the state drained directly by the Mississippi River),
- Tennessee (all but a small part in the extreme
west of the state drained directly by the Mississippi River and a small area in
the southeastern corner of the state which is drained by the Conasauga River),
- Virginia (most of Southwest Virginia),
- North Carolina (the western quarter of the state),
- Georgia (the northwest corner of the state),
- Alabama (the northern portion of the state), and
- Mississippi (the northeast corner of the state).
Geology
The Ohio River is young from a geologic standpoint. 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, and 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 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, the valleys are
actually found on hilltops.[clarify]
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, and eventually the
upper and middle sections combined to form what is essentially the modern Ohio River.
History
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 mere tributary of the Mississippi. 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, though the forks (the
confluence of the Allegheny and Monongahela rivers at what is now Pittsburgh) was considered a strategic military location.
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 both Pennsylvania and Virginia—both of whom 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 --perhaps the world's first truly global conflict --the Seven Years'
War between England and France. After several initial defeats, the British evntually gained sovereignty over the Ohio
Valley.
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 13
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 in about a two-mile stretch. In this area the river flowed over hard,
fossil-rich beds of limestone. The first locks
on the river were built at Louisville to circumnavigate the falls. Today it is the site of McAlpine Locks and Dam.
Because the Ohio River flowed westwardly, it became the 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, killed
them, stole their goods, and scuttled their boats. The folktales of Mike Fink recall the
keelboats used for commerce in the early days of European settlement. In 1843 the Ohio river
boatmen were the inspiration for Dan Emmett's The
Boatman's Dance.
Other boats 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 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 it is the Southern border of Ohio, Indiana and Illinois, the Ohio River was a part of the border that divided free
states and slave states in the years before the American Civil War. The expression
"sold down the river" originated as a lament of Kentucky slaves being split
apart from their families and sold in Louisville and other Kentucky locations to be shipped via the Ohio River down to New
Orleans to be sold yet again to owners of cotton and sugar field plantations.[2][3] Before and during the Civil
War, the Ohio River was called the "River Jordan" by slaves escaping to freedom in the North via the Underground Railroad.[4] As
depicted in several novels by Harriet Beecher Stowe and Toni Morrison. More routes, and more escaping slaves made their perilous journey north to freedom across
the Ohio River, than anywhere else across the north-south frontier. In 1831, in the Ohio River town of Ripley, Ohio, an irate
slave catcher, in hot pursuit, coined the term, 'Underground Railroad,' when his quarry apparently just vanished' in one. Ripley
was a hotbed of abolitionist activity. Runaway slaves were generally welcomed there. And free-to-operate-in-the-north Slave
Catchers also worked openly in Ripley. In Ripley, Eliza was the true life character, of Harriet Beecher Stowe's novel. Eliza and
her baby, crossed the Ohio one winter night, slipping, and cutting her feet as she leaped from one ice floe to the next. Farther
down the river, near Grandview, Indiana, slave Josiah Henson started his daring escape toward freedom with his entire family.
Today, the Ohio River generally separates Midwestern Great Lakes states from Southern border states.
The charter for Virginia went not to the middle of the Ohio River, but to its far shore so
the entire river was included. Wherever the river serves as a boundary between states, the river essentially belongs to the two
states on the south that were divided from Virginia. 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 disputed Illinois' right to collect taxes on a riverboat casino docked in Metropolis, citing their control of the entire river. Aztar opened their own casino riverboat that
docked in Evansville, Indiana at about the same time. Although cruises on the Ohio river were at first done in an oval pattern up
and down the Ohio, the state of Kentucky soon protested and cruises were limited 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 Louisville, Kentucky. In 2006, Cincinnati, Ohio, Indie Rock band Nevada Smith published a bootleg version of their song "Il Fiume Fluisce Colore Maronne", a humorous
protest song against the pollution in the Ohio. In 1993, Louisville band Love Jones
released a song about recreational life on the Ohio River called "Ohio River".
River depth
While the Ohio River is quite deep it is a naturally shallow river that was artificially deepened by series of dams. The dams
raise the water level in shallow stretches, 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 deep all the way past
Cincinnati. From its origin to Cincinnati, the average depth is approximately 27 feet. 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 rivers depth increases nearly fivefold over about 100 miles, coming to a maximum depth of 168 feet just west of Louisville,
Kentucky. The 50 miles around Louisville represent the deepest area of the river with an average depth of approximately 132 feet,
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, due to the fact that it is more
free flowing in the region.
Water levels for the Ohio River are predicted daily by the National Oceanic and Atmospheric Administration (NOAA). The water depth
predictions are relative to each local flood plain based upon predicted rainfall in the Ohio River basin in 5 reports as
follows:
- Pittsburgh, PA to Hannibal Dam, OH (including the Allegheny & Monongahela rivers) (click to see report)
- Willow Island Dam, OH to Greenup Dam, KY (including the Kanawha River) (click to see report)
- Portsmouth, OH to Markland Dam, KY (click to see report)
- McAlpine Dam, KY to Cannelton Dam, IN (click to see report)
- Newburgh Dam, IN to Golconda, IL (click to see report) [5]
Cities and towns
-
Cities along the Ohio include:
Recreation
The world record for the largest blue catfish
taken in the line class (104 lbs.), was set on the Ohio River in 1999. The river also holds records for the following species for
the state of Kentucky:[6]
References
See also
Wikimedia Commons has media related to:
External links
Online maps and aerial photos
Mouth or other endpoint (Mississippi River)
Source (Pittsburgh)
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)