Youtube results:
The Ohio River is the largest tributary, by volume, of the Mississippi River. At the confluence, the Ohio is even bigger than the Mississippi (Ohio at Cairo: 281,500 cu ft/s (7,960 m3/s);[2] Mississippi at Thebes: 208,200 cu ft/s (5,897 m3/s)[3]) and, thus, is hydrologically the main stream of the whole river system, including the Allegheny River further upstream. 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 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, as well as in the Mississippi Valley and the Southeast. 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. Its waters connected communities. The Osage, Omaha, Ponca and Kaw lived in the Ohio Valley, but under pressure from the Iroquois to the northeast, migrated west of the Mississippi River to Missouri, Arkansas, and Oklahoma in the 1600s.
René-Robert Cavelier, Sieur de La Salle led an expedition to the Ohio River in 1669. His French party were the first Europeans to see the river. 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 for pioneers 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 19th century, the river was the southern boundary of the Northwest Territory. It is sometimes considered as the western extension of the Mason–Dixon Line that divided Pennsylvania from Maryland, and thus part of the border between free and slave territory, and between the Northern and Southern United States or Upper South. Where the river was narrow, it was the way to freedom for thousands of slaves escaping to the North, many helped by free blacks and whites of the Underground Railroad resistance movement.
The Ohio River is a climatic transition area, as its water runs along the periphery of the humid subtropical and humid continental climate areas. It is inhabited by fauna and flora of both climates. In winter it regularly freezes over at Pittsburgh but rarely so as it travels further south toward Cincinnati and Louisville. At Paducah, Kentucky in the south, near the Ohio’s confluence with the Mississippi, it is ice-free year round. Paducah was founded there because it is the northernmost ice-free reach of the Ohio. 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."[4]
Contents |
The Allegheny River (left) and Monongahela River (right) join to form the Ohio River at Pittsburgh, Pennsylvania—the largest metropolitan area on the river.
Wheeling, West Virginia, a major city on the river, was the first city to have a bridge across the river.
Louisville, Kentucky is situated at both the widest and deepest level of the Ohio River.
A barge hauling coal in the Louisville and Portland Canal, the only man-made portion of the Ohio River.
Cincinnati, Ohio is a well-known city along the Ohio River, historically known for its riverboats. The Tall Stacks festival celebrates the Cincinnati riverboats and the Ohio River every three or four years.
Evansville, Indiana, the third-largest city in Indiana and the fourth-largest city on the river.
The Ohio River is formed by the confluence of the Allegheny and Monongahela rivers at Point State Park in Pittsburgh, Pennsylvania. From there, it flows northwest through Allegheny and 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 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. Its course forms the northern borders of West Virginia and Kentucky; and the southern borders of Ohio, Indiana and Illinois, until it joins the Mississippi River near the city of Cairo, Illinois.
Major tributaries of the river, indicated by the location of the mouths, include:
The Ohio's drainage basin covers 189,422 square miles (490,600 km2), encompassing the easternmost regions of the Mississippi Basin. The Ohio drains parts of 15 states in four regions.
From a geological 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.
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]
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, creating a large lake until the dam burst. A new route was carved to the Mississippi. Eventually the upper and middle sections combined to form what is essentially the modern Ohio River.
Pre-Columbian inhabitants of eastern North America considered the Ohio part of a single river continuing on through the lower Mississippi. The river's name comes from the Seneca (Iroquoian) ohiːyo', a proper name derived from ohiːyoːh, meaning "good river".[5] The river is 1,310 miles (2,110 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 also 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 at present-day Louisville 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. La Salle claimed the Ohio Valley for France.
French fur traders operated in the area, and France built forts along the Allegheny River.
In 1749, Great Britain established the Ohio Company to settle and trade in the area. 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 the French. In 1763, following the Seven Years War, France ceded the area to Britain.
The 1768 Treaty of Fort Stanwix opened Kentucky to colonial settlement and established the Ohio River as a southern boundary for American Indian territory.[6] 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 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, operating out of 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 states 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 shipped via the Ohio and Mississippi to cotton and sugar plantations in the Deep South.[7][8] 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.[9] More escaping slaves, estimated in the thousands, made their perilous journey north to freedom across the Ohio River than anywhere else across the north-south frontier. Harriet Beecher Stowe's Uncle Tom's Cabin, the bestselling novel that fueled abolitionist work, was the best known of the anti-slavery novels that portrayed such escapes across the Ohio. The times have been expressed by 20th-century novelists as well, such as the Nobel Prize-winning Toni Morrison, whose novel Beloved was adapted as a film of the same name. She also composed the libretto for the opera Margaret Garner (2005), based on the life and trial of an enslaved woman who escaped with her family across the river.
The Ohio River is considered to separate Midwestern Great Lakes states from the Upper South states, which were historically border states in the Civil War.
The colonial charter for Virginia defined its territory as extending to the north shore of the Ohio, so that the riverbed was "owned" by Virginia. Where the river serves as a boundary between states today, Congress designated the entire river to belong to the states on the east and south, i.e., West Virginia and Kentucky at the time of admission to the Union, that were divided from Virginia. Thus Wheeling Island, the largest inhabited island in the Ohio River, belongs to West Virginia, although 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. Since 2002, Indiana has allowed its riverboat casinos to be permanently docked.
In the early 1980s, the Falls of the Ohio National Wildlife Conservation Area was established at Clarksville, Indiana.
The confluence of the Mississippi and Ohio rivers is 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 on December 15, 1967, killing 46 persons.
Mouth of the Ohio, as it feeds into the Mississippi.
Cave-in-rock, view on the Ohio (circa 1832): aquatint by Karl Bodmer from the book "Maximilian, Prince of Wied’s Travels in the Interior of North America, during the years 1832–1834"
The Ohio River is a naturally shallow river that was artificially deepened by a series of dams. The natural depth of the river varied from about 3 to 20 feet (0.91 to 6.1 m). 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. From its origin to Cincinnati, the average depth is approximately 15 feet (5 m). The maximum depth is below the McAlpine Locks and Dam at the Falls of the Ohio at Louisville, Kentucky, where flood stage is reached when the water reaches 23 feet (7 m) on the lower gauge. From Louisville, the river loses depth very gradually until its confluence with the Mississippi at Cairo, Illinois, where it has an approximate depth of 19 feet (6 m).
Water levels for the Ohio River from Smithland Lock and Dam upstream to Pittsburgh are predicted daily by the National Oceanic and Atmospheric Administration's Ohio River Forecast Center. The water levels for the Ohio River from Smithland Lock and Dam to Cairo, Illinois, are predicted by the National Oceanic and Atmospheric Administration's Lower Mississippi 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:
Metro Area | Population |
---|---|
Pittsburgh | 2.4 million |
Cincinnati | 2.2 million |
Louisville | 1.4 million |
Evansville | 358,000 |
Huntington-Ashland | 290,000 |
Parkersburg | 160,000 |
Wheeling | 145,000 |
Weirton-Steubenville | 132,000 |
Owensboro | 112,000 |
Cities along the Ohio include:
|
The world record for the largest blue catfish 104 pounds (47.2 kg) 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:[11]
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]
This article's use of external links may not follow Wikipedia's policies or guidelines. Please improve this article by removing excessive or inappropriate external links, and converting useful links where appropriate into footnote references. (September 2010) |
Wikisource has original works written by or about: |
Wikimedia Commons has media related to: Ohio River |
State of Ohio | |||||
|
|||||
Nickname(s): The Buckeye State; The Mother of Presidents; Birthplace of Aviation; The Heart of It All |
|||||
Motto(s): With God, all things are possible | |||||
Official language(s) | None. (English, de facto) | ||||
Demonym | Ohioan; Buckeye[1] (colloq.) | ||||
Capital (and largest city) |
Columbus[2][3] | ||||
Largest metro area | Greater Cleveland or Greater Cincinnati (see footnote[4]) |
||||
Area | Ranked 34th in the U.S. | ||||
- Total | 44,825 sq mi (116,096 km2) |
||||
- Width | 220 miles (355 km) | ||||
- Length | 220 miles (355 km) | ||||
- % water | 8.7 | ||||
- Latitude | 38° 24′ N to 41° 59′ N | ||||
- Longitude | 80° 31′ W to 84° 49′ W | ||||
Population | Ranked 7th in the U.S. | ||||
- Total | 11,544,951 (2011 est)[5] | ||||
- Density | 282/sq mi (109/km2) Ranked 10th in the U.S. |
||||
Elevation | |||||
- Highest point | Campbell Hill[6][7] 1,549 ft (472 m) |
||||
- Mean | 850 ft (260 m) | ||||
- Lowest point | Ohio River at Indiana border[6][7] 455 ft (139 m) |
||||
Before statehood | Northwest Territory | ||||
Admission to Union | March 1, 1803[8] (17th, declared retroactively on August 7, 1953[9]) |
||||
Governor | John Kasich[10] (R)[11] | ||||
Lieutenant Governor | Mary Taylor[12] (R)[13] | ||||
Legislature | General Assembly | ||||
- Upper house | Senate | ||||
- Lower house | House of Representatives | ||||
U.S. Senators | Sherrod Brown[14] (D)[14] Rob Portman (R) |
||||
U.S. House delegation | 13 Republicans, 5 Democrats (list) | ||||
Time zone | Eastern: UTC-5/-4 | ||||
Abbreviations | OH[15] US-OH | ||||
Website | www.ohio.gov |
Ohio (i/oʊˈhaɪ.oʊ/) is a state in the Midwestern United States. Ohio is the 34th most extensive, the 7th most populous, and the 10th most densely populated of the 50 United States. The state's capital and largest city is Columbus.
The name "Ohio" originated from Iroquois word ohi-yo’, meaning "great river".[16][17][18][19][20] The state, originally partitioned from the Northwest Territory, was admitted to the Union as the 17th state (and the first under the Northwest Ordinance) on March 1, 1803.[8][21] Although there are conflicting narratives regarding the origin of the nickname, Ohio is historically known as the "Buckeye State" (relating to the Ohio buckeye tree) and Ohioans are also known as "Buckeyes".[1]
The government of Ohio is composed of the executive branch, led by the Governor; the legislative branch, which comprises the Ohio General Assembly; and the judicial branch, which is led by the Supreme Court. Currently, Ohio occupies 18 seats in the United States House of Representatives.[22] Ohio is known for its status as both a swing state[23] and a bellwether[23] in national elections.
Contents |
Ohio's geographic location has proven to be an asset for economic growth and expansion. Because Ohio links the Northeast to the Midwest, much cargo and business traffic passes through its borders along its well-developed highways. Ohio has the nation's 10th largest highway network, and is within a one-day drive of 50% of North America's population and 70% of North America's manufacturing capacity.[24] To the north, Lake Erie gives Ohio 312 miles (502 km) of coastline,[25] which allows for numerous seaports. Ohio's southern border is defined by the Ohio River (with the border being at the 1793 low-water mark on the north side of the river), and much of the northern border is defined by Lake Erie. Ohio's neighbors are Pennsylvania to the east, Michigan to the northwest, Ontario Canada, to the north, Indiana to the west, Kentucky on the south, and West Virginia on the southeast. Ohio's borders were defined by metes and bounds in the Enabling Act of 1802 as follows:
Bounded on the east by the Pennsylvania line, on the south by the Ohio River, to the mouth of the Great Miami River, on the west by the line drawn due north from the mouth of the Great Miami aforesaid, and on the north by an east and west line drawn through the southerly extreme of Lake Michigan, running east after intersecting the due north line aforesaid, from the mouth of the Great Miami until it shall intersect Lake Erie or the territorial line, and thence with the same through Lake Erie to the Pennsylvania line aforesaid.
Note that Ohio is bounded by the Ohio River, but nearly all of the river itself belongs to Kentucky and West Virginia. In 1980, the U.S. Supreme Court held that, based on the wording of the cessation of territory by Virginia (which, at that time included what is now Kentucky and West Virginia), the boundary between Ohio and Kentucky (and by implication, West Virginia) is the northern low-water mark of the river as it existed in 1792.[26] Ohio has only that portion of the river between the river's 1792 low-water mark and the present high-water mark.
The border with Michigan has also changed, as a result of the Toledo War, to angle slightly northeast to the north shore of the mouth of the Maumee River.
Much of Ohio features glaciated plains, with an exceptionally flat area in the northwest being known as the Great Black Swamp. This glaciated region in the northwest and central state is bordered to the east and southeast first by a belt known as the glaciated Allegheny Plateau, and then by another belt known as the unglaciated Allegheny Plateau. Most of Ohio is of low relief, but the unglaciated Allegheny Plateau features rugged hills and forests.
The rugged southeastern quadrant of Ohio, stretching in an outward bow-like arc along the Ohio River from the West Virginia Panhandle to the outskirts of Cincinnati, forms a distinct socio-economic unit. Geologically similar to parts of West Virginia and southwestern Pennsylvania, this area's coal mining legacy, dependence on small pockets of old manufacturing establishments, and distinctive regional dialect set this section off from the rest of the state. In 1965 the United States Congress passed the Appalachian Regional Development Act, at attempt to "address the persistent poverty and growing economic despair of the Appalachian Region."[27] This act defines 29 Ohio counties as part of Appalachia.[28] While 1/3 of Ohio's land mass is part of the federally defined Appalachian region, only 12.8% of Ohioans live there (1.476 million people.)[29]
Significant rivers within the state include the Cuyahoga River, Great Miami River, Maumee River, Muskingum River, and Scioto River. The rivers in the northern part of the state drain into the northern Atlantic Ocean via Lake Erie and the St. Lawrence River, and the rivers in the southern part of the state drain into the Gulf of Mexico via the Ohio River and then the Mississippi.
The worst weather disaster in Ohio history occurred along the Great Miami River in 1913. Known as the Great Dayton Flood, the entire Miami River watershed flooded, including the downtown business district of Dayton. As a result, the Miami Conservancy District was created as the first major flood plain engineering project in Ohio and the United States.[30]
Grand Lake St. Marys in the west central part of the state was constructed as a supply of water for canals in the canal-building era of 1820–1850. For many years this body of water, over 20 square miles (52 km2), was the largest artificial lake in the world. It should be noted that Ohio's canal-building projects were not the economic fiasco that similar efforts were in other states. Some cities, such as Dayton, owe their industrial emergence to location on canals, and as late as 1910 interior canals carried much of the bulk freight of the state.
The climate of Ohio is a humid continental climate (Koppen climate classification Dfa) throughout most of the state except in the extreme southern counties of Ohio's Bluegrass region section which are located on the northern periphery of the humid subtropical climate and Upland South region of the United States. Summers are typically hot and humid throughout the state, while winters generally range from cool to cold. Precipitation in Ohio is moderate year-round. Severe weather is not uncommon in the state, although there are typically fewer tornado reports in Ohio than in states located in what is known as the Tornado Alley. Severe lake effect snowstorms are also not uncommon on the southeast shore of Lake Erie, which is located in an area designated as the Snowbelt.
Although predominantly not in a subtropical climate, some warmer-climate flora and fauna does reach well into Ohio. For instance, a number of trees with more southern ranges, such as the blackjack oak, Quercus marilandica, are found at their northernmost in Ohio just north of the Ohio River. Also evidencing this climatic transition from a subtropical to continental climate, several plants such as the Southern magnolia (Magnolia grandiflora), Albizia julibrissin (mimosa), Crape Myrtle, and even the occasional Needle Palm are hardy landscape materials regularly used as street, yard, and garden plantings in the Bluegrass region of Ohio; but these same plants will simply not thrive in much of the rest of the State. This interesting change may be observed while traveling through Ohio on Interstate 75 from Cincinnati to Toledo; the observant traveler of this diverse state may even catch a glimpse of Cincinnati's common wall lizard, one of the few examples of permanent "subtropical" fauna in Ohio.
The highest recorded temperature was 113 °F (45 °C), near Gallipolis on July 21, 1934.[31] The lowest recorded temperature was −39 °F (−39 °C), at Milligan on February 10, 1899.[32]
Although few have registered as noticeable to the average citizen, more than 30 earthquakes occurred in Ohio between 2002 and 2007, and more than 200 quakes with a magnitude of 2.0 or higher have occurred since 1776.[33]
The most substantial known earthquake in Ohio history was the Anna (Shelby County) earthquake,[34] which occurred on March 9, 1937. It was centered in western Ohio, and had a magnitude of 5.4, and was of intensity VIII.[35]
Other significant earthquakes in Ohio include:[36] one of magnitude 4.8 near Lima on September 19, 1884;[37] one of magnitude 4.2 near Portsmouth on May 17, 1901;[38] and one of 5.0 in LeRoy Township in Lake County on January 31, 1986, which continued to trigger 13 aftershocks of magnitude 0.5 to 2.4 for two months.[39][40]
The most recent earthquake in Ohio of any appreciable magnitude occurred on December 31, 2011, at 3:05pm EST. It had a magnitude of 4.0, and its epicenter was located approximately 4 kilometres northwest of Youngstown (41°7′19.1994″N 80°41′2.3994″W / 41.121999833°N 80.683999833°W / 41.121999833; -80.683999833), near the Trumbull/Mahoning county border.[41]
The Ohio Seismic Network (OhioSeis), a group of seismograph stations at several colleges, universities, and other institutions, and coordinated by the Division of Geological Survey of the Ohio Department of Natural Resources,[42] maintains an extensive catalog of Ohio earthquakes from 1776 to the present day, as well as earthquakes located in other states whose effects were felt in Ohio.[43]
Rank | City | 2010 Population[44] | 2010 Metro Population[45] |
---|---|---|---|
1 | Columbus | 787,033 | 1,836,540 |
2 | Cleveland | 396,815 | 2,077,240 |
3 | Cincinnati | 296,943 | 2,130,151 |
4 | Toledo | 287,208 | 651,429 |
5 | Akron | 199,110 | 703,200 |
6 | Dayton | 141,527 | 841,502 |
7 | Parma | 81,601 | 1 |
8 | Canton | 73,007 | 404,422 |
9 | Youngstown | 66,982 | 565,773 |
10 | Lorain | 64,097 | 1 |
11 | Hamilton | 62,477 | 2 |
12 | Springfield | 60,608 | 133,333 |
13 | Kettering | 56,163 | 4 |
14 | Elyria | 54,533 | 1 |
15 | Lakewood | 52,131 | 1 |
16 | Cuyahoga Falls | 49,652 | 5 |
17 | Euclid | 48,920 | 1 |
18 | Middletown | 48,694 | 2 |
19 | Mansfield | 47,821 | 124,475 |
20 | Newark | 47,573 | 3 |
|
Columbus (home of The Ohio State University, Franklin University, Capital University, and Ohio Dominican University) is the capital of Ohio, near the geographic center of the state.
Other Ohio cities functioning as centers of United States metropolitan areas include:
Note: The Cincinnati metropolitan area extends into Kentucky and Indiana, the Steubenville metropolitan area extends into West Virginia, and the Youngstown metropolitan area extends into Pennsylvania.
Ohio cities that function as centers of United States micropolitan areas include:
Archeological evidence suggests that the Ohio Valley was inhabited by nomadic people as early as 13,000 BC.[46] These early nomads disappeared from Ohio by 1,000 BC, "but their material culture provided a base for those who followed them".[46] Between 1,000 and 800 BC, the sedentary Adena culture emerged. As Ohio historian George W. Knepper notes, this sophisticated culture was "so named because evidences of their culture were excavated in 1902 on the grounds of Adena, Thomas Worthington's estate located near Chillicothe".[47] The Adena were able to establish "semi-permanent" villages because they domesticated plants, which included squash, sunflowers, and perhaps corn. Cultivation of these in addition to hunting and gathering supported more settled, complex villages.[47] The most spectacular remnant of the Adena culture is the Great Serpent Mound, located in Adams County, Ohio.[47]
Around 100 BC, the Adena were joined in Ohio Country by the Hopewell people, who were named for the farm owned by Captain M. C. Hopewell, where evidence of their unique culture was discovered.[48] Like the Adena, the Hopewell people participated in a mound-building culture. Their complex, large and technologically sophisticated earthworks can be found in modern-day Marietta, Newark, and Circleville.[48] The Hopewell, however, disappeared from the Ohio Valley in about 600 AD. Little is known about the people who replaced them.[49] Researchers have identified two additional, distinct prehistoric cultures: the Fort Ancient people and the Whittlesey Focus people.[49] Both cultures apparently disappeared in the 17th century, perhaps decimated by infectious diseases spread in epidemics from early European contact. The Native Americans had no immunity to common European diseases. Some scholars believe that the Fort Ancient people "were ancestors of the historic Shawnee people, or that, at the very least, the historic Shawnees absorbed remnants of these older peoples."[49]
American Indians in the Ohio Valley were greatly affected by the aggressive tactics of the Iroquois Confederation, based in central and western New York.[50] After the so-called Beaver Wars in the mid-17th century, the Iroquois claimed much of the Ohio country as hunting and, more importantly, beaver-trapping ground. After the devastation of epidemics and war in the mid-17th century, which largely emptied the Ohio country of indigenous people by the mid-to-late 17th century, the land gradually became repopulated by the mostly Algonquian-speaking descendants of its ancient inhabitants, that is, descendants of the Adena, Hopewell, and Mississippian cultures. Many of these Ohio-country nations were multi-ethnic (sometimes multi-linguistic) societies born out of the earlier devastation brought about by disease, war, and subsequent social instability. They subsisted on agriculture (corn, sunflowers, beans, etc.) supplemented by seasonal hunts. By the 18th century, they were part of a larger global economy brought about by European entry into the fur trade.[51]
The indigenous nations to inhabit Ohio in the historical period included the Miamis (a large confederation); Wyandots (made up of refugees, especially from the fractured Huron confederacy); Delawares (pushed west from their historic homeland in New Jersey); Shawnees (also pushed west, although they may have been descended from the Fort Ancient people of Ohio); Ottawas (more commonly associated with the upper Great Lakes region); Mingos (like the Wyandot, a group recently formed of refugees from Iroquois); and Eries (gradually absorbed into the new, multi-ethnic "republics," namely the Wyandot).[52] Ohio country was also the site of Indian massacres, such as the Yellow Creek Massacre, Gnadenhutten and Pontiac's Rebellion school massacre.[53]
During the 18th century, the French set up a system of trading posts to control the fur trade in the region. In 1754, France and Great Britain fought a war that was known in North America as the French and Indian War and in Europe as the Seven Years War. As a result of the Treaty of Paris, the French ceded control of Ohio and the remainder of the Old Northwest to Great Britain.
Pontiac's Rebellion in the 1760s, however, posed a challenge to British military control.[54] This came to an end with the colonists' victory in the American Revolution. In the Treaty of Paris in 1783, Britain ceded all claims to Ohio country to the United States.
The United States created the Northwest Territory under the Northwest Ordinance of 1787.[55] Slavery was not permitted in the new territory. Settlement began with the founding of Marietta by the Ohio Company of Associates, which had been formed by a group of American Revolutionary War veterans. Following the Ohio Company, the Miami Company (also referred to as the "Symmes Purchase") claimed the southwestern section, and the Connecticut Land Company surveyed and settled the Connecticut Western Reserve in present-day Northeast Ohio.
The old Northwest Territory originally included areas previously known as Ohio Country and Illinois Country. As Ohio prepared for statehood, the Indiana Territory was created, reducing the Northwest Territory to approximately the size of present-day Ohio plus the eastern half of the Lower Peninsula of Michigan and the eastern tip of the Upper Peninsula.
Under the Northwest Ordinance, areas of the territory could be defined and admitted as states once their population reached 60,000. Although Ohio's population numbered only 45,000 in December 1801, Congress determined that the population was growing rapidly and Ohio could begin the path to statehood. The assumption was that it would exceed 60,000 residents by the time it was admitted as a state.
On February 19, 1803, President Jefferson signed an act of Congress that approved Ohio's boundaries and constitution. However, Congress had never passed a resolution formally admitting Ohio as the 17th state. The current custom of Congress declaring an official date of statehood did not begin until 1812, with Louisiana's admission as the 18th state. Although no formal resolution of admission was required, when the oversight was discovered in 1953, Ohio congressman George H. Bender introduced a bill in Congress to admit Ohio to the Union retroactive to March 1, 1803. At a special session at the old state capital in Chillicothe, the Ohio state legislature approved a new petition for statehood that was delivered to Washington, D.C. on horseback. On August 7, 1953 (the year of Ohio's 150th anniversary), President Eisenhower signed an act that officially declared March 1, 1803 the date of Ohio's admittance into the Union.[56][57]
Although many Native Americans had migrated west to evade American encroachment, others remained settled in the state, sometimes assimilating in part. In 1830 under President Andrew Jackson, the US government forced Indian Removal of most tribes to the Indian Territory west of the Mississippi River.
In 1835, Ohio fought with Michigan in the Toledo War, a mostly bloodless boundary war over the Toledo Strip. Congress intervened, making Michigan's admittance as a state conditional on ending the conflict. In exchange for giving up its claim to the Toledo Strip, Michigan was given the western two-thirds of the Upper Peninsula, in addition to the eastern third that was already considered part of the state.
Ohio's central position and its population gave it an important place during the Civil War. The Ohio River was a vital artery for troop and supply movements, as were Ohio's railroads. Ohio contributed more soldiers per-capita than any other state in the Union. In 1862, the state's morale was badly shaken in the aftermath of the battle of Shiloh, a costly victory in which Ohio forces suffered 2,000 casualties.[58] Later that year, when Confederate troops under the leadership of Stonewall Jackson threatened Washington, D.C., Ohio governor David Tod still could recruit 5,000 volunteers to provide three months of service.[59] Ohio historian Andrew R. L. Cayton writes that almost 35,000 Ohioans died in the conflict, "and some thirty thousand carried battle scars with them for the rest of their lives."[60] By the end of the Civil War, the Union's top three generals–Ulysses S. Grant, William Tecumseh Sherman, and Philip Sheridan–were all from Ohio.[61][62]
In 1912 a Constitutional Convention was held with Charles B. Galbreath as secretary. The result reflected the concerns of the Progressive Era. It introduced the initiative and the referendum. In addition, it allowed the General Assembly to put questions on the ballot for the people to ratify laws and constitutional amendments originating in the Legislature. Under the Jeffersonian principle that laws should be reviewed once a generation, the constitution provided for a recurring question to appear on Ohio's general election ballots every 20 years. The question asks whether a new convention is required. Although the question has appeared in 1932, 1952, 1972, and 1992, it has never been approved. Instead constitutional amendments have been proposed by petition to the legislature hundreds of times and adopted in a majority of cases.
Eight U.S. presidents hailed from Ohio at the time of their elections, giving rise to its nickname "Mother of Presidents", a sobriquet it shares with Virginia. It is also termed "Modern Mother of Presidents,"[63] in contrast to Virginia's status as the origin of presidents earlier in American history. Seven presidents were born in Ohio, making it second to Virginia's eight. Virginia-born William Henry Harrison lived most of his life in Ohio and is also buried there. Harrison conducted his political career while living on the family compound, founded by his father-in-law, John Cleves Symmes, in North Bend, Ohio. The seven presidents born in Ohio were Ulysses S. Grant, Rutherford B. Hayes, James A. Garfield, Benjamin Harrison (grandson of William Henry Harrison), William McKinley, William Howard Taft and Warren G. Harding.
Historical populations | |||
---|---|---|---|
Census | Pop. | %± | |
1800 | 45,365 |
|
|
1810 | 230,760 | 408.7% | |
1820 | 581,434 | 152.0% | |
1830 | 937,903 | 61.3% | |
1840 | 1,519,467 | 62.0% | |
1850 | 1,980,329 | 30.3% | |
1860 | 2,339,511 | 18.1% | |
1870 | 2,665,260 | 13.9% | |
1880 | 3,198,062 | 20.0% | |
1890 | 3,672,329 | 14.8% | |
1900 | 4,157,545 | 13.2% | |
1910 | 4,767,121 | 14.7% | |
1920 | 5,759,394 | 20.8% | |
1930 | 6,646,697 | 15.4% | |
1940 | 6,907,612 | 3.9% | |
1950 | 7,946,627 | 15.0% | |
1960 | 9,706,397 | 22.1% | |
1970 | 10,652,017 | 9.7% | |
1980 | 10,797,630 | 1.4% | |
1990 | 10,847,115 | 0.5% | |
2000 | 11,353,140 | 4.7% | |
2010 | 11,536,504 | 1.6% | |
Source: 1910–2010[64] |
By race | White | Black | AIAN* | Asian | NHPI* |
---|---|---|---|---|---|
2000 (total population) | 86.83% | 12.18% | 0.67% | 1.41% | 0.06% |
2000 (Hispanic only) | 1.70% | 0.19% | 0.05% | 0.02% | 0.01% |
2005 (total population) | 86.27% | 12.66% | 0.66% | 1.68% | 0.07% |
2005 (Hispanic only) | 2.05% | 0.20% | 0.05% | 0.03% | 0.01% |
Growth 2000–05 (total population) | 0.32% | 4.98% | -1.57% | 20.32% | 9.32% |
Growth 2000–05 (non-Hispanic only) | -0.11% | 4.97% | -1.96% | 20.48% | 11.15% |
Growth 2000–05 (Hispanic only) | 22.11% | 5.70% | 3.04% | 10.81% | -0.26% |
* AIAN is American Indian or Alaskan Native; NHPI is Native Hawaiian or Pacific Islander |
From just over 45,000 residents in 1800, Ohio's population grew at rates of over 10% per decade until the census of 1970, which recorded just over 10.65 million Ohioans.[65] Growth then slowed for the next four decades.[66] The United States Census Bureau estimates that the population of Ohio was 11,544,951 on July 1, 2011, a 0.07% increase since the 2010 United States Census.[5] Ohio's population growth lags that of the entire United States, and Caucasians are found in a greater density than the United States average. As of 2000[update], Ohio's center of population is located in Morrow County,[67] in the county seat of Mount Gilead.[68] This is approximately 6,346 feet (1,934 m) south and west of Ohio's population center in 1990.[67]
As of 2007[update], 6.5% of Ohio's population is under 5 years of age,[69] compared to a national rate of 6.9%.[70] Also, 13.4% of Ohio's population is over 65 years of age,[69] compared to a United States rate of 12.6%.[70] Females comprise 51.3% of Ohio's population,[69] compared to a national rate of 50.8%.[70]
As of 2007, 3.6% of Ohio's total population is estimated to be foreign-born,[71] compared to an estimated 12.5% of the United States population.[71]
Ohio's five largest ancestry groups, as of 2007, are:[72]
The American Community Survey for the U.S. Census for 2006 reported:[73]
According to a Pew Forum poll, as of 2008, 76% of Ohioans identified as Christian.[74] Specifically, 26% of Ohio's population identified as Evangelical Protestant, 22% identified as Mainline Protestant, and 21% identified as Roman Catholic.[74] In addition, 17% of the population is unaffiliated with any religious body.[74] There are also small minorities of Jehovah's Witnesses (1%), Jews (1%), Muslims (1%), Hindus (<0.5%), Buddhists (<0.5%), Mormons (<0.5%), and practitioners of other faiths (1-1.5%).[74]
According to the same data, a majority of Ohioans, 55%, feel that religion is "very important," while 30% say that it is "somewhat important," and 15% responded that religion is "not too important/not important at all."[74] Also, 36% of Ohioans indicate that they attend religious services at least once weekly, while 35% attend these services occasionally, and 27% seldom or never participate in these services.[74]
In 2010, Ohio was ranked No. 2 in the country for best business climate by Site Selection magazine, based on a business-activity database.[75] The state has also won three consecutive Governor's Cup awards from the magazine, based on business growth and developments.[76] As of 2010[update], Ohio's gross domestic product (GDP) was $478 billion.[77][78] This ranks Ohio's economy as the seventh-largest of all fifty states and the District of Columbia.[78]
The Small Business & Entrepreneurship Council ranked the state No. 10 for best business-friendly tax systems in their Business Tax Index 2009, including a top corporate tax and capital gains rate that were both ranked No. 6 at 1.9%.[79] Ohio was ranked No. 11 by the council for best friendly-policy states according to their Small Business Survival Index 2009.[80] The Directorship's Boardroom Guide ranked the state No. 13 overall for best business climate, including No. 7 for best litigation climate.[81] Forbes ranked the state No. 8 for best regulatory environment in 2009.[82] Ohio has 5 of the top 115 colleges in the nation, according to U.S. News and World Report's 2010 rankings,[83] and was ranked No. 8 by the same magazine in 2008 for best high schools.[84]
Ohio's unemployment rate stood at 10.7 in May 2010, adding 17,000 new jobs that month.[85][86] Ohio's per capita income stands at $34,874.[78][87] Moody's is predicting a 1.3% increase in personal income in 2009 for Ohio, compared to the 2007 rate of 4.7%.[78] As of 2007[update], Ohio's median household income is $46,645,[88] and 13.1% of the population is below the poverty line,[89] slightly above the national rate of 13%.[89] Ohio's employment base is expected to grow 5% from 2006 to 2016, a net gain of 290,700 jobs.[78]
The manufacturing and financial activities sectors each compose 18.3% of Ohio's GDP, making them Ohio's largest industries by percentage of GDP.[78] Ohio has the largest bioscience sector in the Midwest, and is a national leader in the "green" economy. Ohio is the largest producer in the country of plastics, rubber, fabricated metals, electrical equipment, and appliances.[90] 5,212,000 Ohioans are currently employed by wage or salary.[78]
By employment, Ohio's largest sector is trade/transportation/utilities, which employs 1,010,000 Ohioans, or 19.4% of Ohio's workforce, while the health care and education sector employs 825,000 Ohioans (15.8%).[78] Government employs 787,000 Ohioans (15.1%), manufacturing employs 669,000 Ohioans (12.9%), and professional and technical services employs 638,000 Ohioans (12.2%).[78] Ohio's manufacturing sector is the third-largest of all fifty United States states in terms of gross domestic product.[78] Fifty-nine of the United States' top 1,000 publicly traded companies (by revenue in 2008) are headquartered in Ohio, including Procter & Gamble, Goodyear Tire & Rubber, AK Steel, Timken, Abercrombie & Fitch, and Wendy's.[91]
Ohio is also one of 41 states with its own lottery,[92] the Ohio Lottery.[93] The Ohio Lottery has contributed over $15.5 billion to public education in its 34-year history.[94]
Ground Travel
Many major east-west transportation corridors go through Ohio. One of those pioneer routes, known in the early 20th century as "Main Market Route 3", was chosen in 1913 to become part of the historic Lincoln Highway which was the first road across America, connecting New York City to San Francisco. In Ohio, the Lincoln Highway linked many towns and cities together, including Canton, Mansfield, Wooster, Lima, and Van Wert. The arrival of the Lincoln Highway to Ohio was a major influence on the development of the state. Upon the advent of the federal numbered highway system in 1926, the Lincoln Highway through Ohio became U.S. Highway 30.
Ohio also is home to 228 miles (367 km) of the Historic National Road, now U.S. Route 40.
Ohio has a highly developed network of roads and interstate highways. Major east-west through routes include the Ohio Turnpike (I-80/I-90) in the north, I-76 through Akron to Pennsylvania, I-70 through Columbus and Dayton, and the Appalachian Highway (Ohio 32) running from West Virginia to Cincinnati. Major north-south routes include I-75 in the west through Toledo, Dayton, and Cincinnati, I-71 through the middle of the state from Cleveland through Columbus and Cincinnati into Kentucky, and I-77 in the eastern part of the state from Cleveland through Akron, Canton, New Philadelphia and Marietta down into West Virginia. Interstate 75 between Cincinnati and Dayton is one of the heaviest traveled sections of interstate in Ohio.
Air Travel
Ohio has 5 international airports, 4 commercial and 2 military. The 5 international includes Cleveland Hopkins International Airport, which is a major hub for Continental Airlines, Port Columbus International Airport, and Dayton International Airport, Ohio's third largest airport. Akron Fulton International Airport handles cargo and for private use. Rickenbacker International Airport is one of military which is also home to the 7th largest fed ex building in America. The other military airport is Wright Patterson Air Force Base which is one of the largest Air Force bases in the United States. Other major airports are located in Toledo and Akron.
Cincinnati/Northern Kentucky International Airport is in Hebron, Kentucky and therefore is not listed above.
The state government of Ohio consists of the executive,[95] judicial,[96] and legislative[97] branches.
The executive branch is headed by the Governor of Ohio.[95] The current governor is John Kasich,[10] a Republican elected in 2010. A lieutenant governor succeeds the governor in the event of any removal from office,[98] and performs any duties assigned by the governor.[99] The current lieutenant governor is Mary Taylor. The other elected constitutional offices in the executive branch are the secretary of state (Jon A. Husted), auditor (Dave Yost), treasurer (Josh Mandel), and attorney general (Mike DeWine).[95]
There are three levels of the Ohio state judiciary. The lowest level is the court of common pleas: each county maintains its own constitutionally-mandated court of common pleas, which maintain jurisdiction over "all justiciable matters."[100] The intermediate-level court system is the district court system.[101] Twelve courts of appeals exist, each retaining jurisdiction over appeals from common pleas, municipal, and county courts in a set geographical area.[100] A case heard in this system is decided by a three-judge panel, and each judge is elected.[100]
The highest-ranking court, the Ohio Supreme Court, is Ohio's "court of last resort."[102] A seven-justice panel composes the court, which, by its own discretion, hears appeals from the courts of appeals, and retains original jurisdiction over limited matters.[103]
The Ohio General Assembly is a bicameral legislature consisting of the Senate and House of Representatives.[105] The Senate is composed of 33 districts, each of which is represented by one senator.[106] Each senator represents approximately 330,000 constituents.[106] The House of Representatives is composed of 99 members.[107]
Year | Republican | Democratic |
---|---|---|
2008 | 46.80% 2,677,820 | 51.38% 2,940,044 |
2004 | 50.81% 2,859,768 | 48.71% 2,741,167 |
2000 | 49.97% 2,351,209 | 46.46% 2,186,190 |
1996 | 41.02% 1,859,883 | 47.38% 2,148,222 |
1992 | 38.35% 1,894,310 | 40.18% 1,984,942 |
1988 | 55.00% 2,416,549 | 44.15% 1,939,629 |
1984 | 58.90% 2,678,560 | 40.14% 1,825,440 |
1980 | 51.51% 2,206,545 | 40.91% 1,752,414 |
1976 | 48.65% 2,000,505 | 48.92% 2,011,621 |
1972 | 59.63% 2,441,827 | 38.07% 1,558,889 |
1968 | 45.23% 1,791,014 | 42.95% 1,700,586 |
1964 | 37.06% 1,470,865 | 62.94% 2,498,331 |
1960 | 53.28% 2,217,611 | 46.72% 1,944,248 |
Ohio, nicknamed the "Mother of Presidents," has sent seven of its native sons (Ulysses S. Grant, Rutherford B. Hayes, James A. Garfield, Benjamin Harrison, William McKinley, William Howard Taft, and Warren G. Harding) to the White House.[109] All seven were Republicans. Virginia native William Henry Harrison, a Whig, resided in Ohio.[109] Historian R. Douglas Hurt asserts that not since Virginia 'had a state made such a mark on national political affairs.'[110] The Economist notes that "This slice of the mid-west contains a bit of everything American — part north-eastern and part southern, part urban and part rural, part hardscrabble poverty and part booming suburb,"[111]
As of 2008[update], Ohio's voter demographic leans towards the Democratic Party.[112] An estimated 2,408,178 Ohioans are registered to vote as Democrats, while 1,471,465 Ohioans are registered to vote as Republicans.[112] These are changes from 2004 of 72% and 32%, respectively, and Democrats have registered over 1,000,000 new Ohioans since 2004.[112] Unaffiliated voters have an attrition of 15% since 2004, losing an estimated 718,000 of their kind.[112] The total now rests at 4,057,518 Ohioans.[112] In total, there are 7,937,161 Ohioans registered to vote.[112] In the United States presidential election of 2008, then-Senator Barack Obama of Illinois won 51.50% of Ohio's popular vote, 4.59% more than his nearest rival, Senator John McCain of Arizona.[113] However, Obama won only 22 of Ohio's 88 counties.[114]
Following the 2000 census, Ohio lost one congressional district in the United States House of Representatives, which leaves Ohio with 18 districts, and consequently, 18 representatives. The state is expected to lose two more seats following the 2010 Census.[115] The 2008 elections, Democrats gained three seats in Ohio's delegation to the House of Representatives.[116] This leaves eight Republican-controlled seats in the Ohio delegation.[117] Ohio's U.S. Senators in the 112th Congress are Republican Rob Portman and Democrat Sherrod Brown.[118] Marcia Kaptur (D-9) is the dean, or most senior member, of the Ohio delegation to the United States House of Representatives.[119]
Ohio's system of public education is outlined in Article VI of the state constitution, and in Title XXXIII of the Ohio Revised Code. Substantively, Ohio's system is similar to those found in other states. At the State level, the Ohio Department of Education, which is overseen by the Ohio State Board of Education, governs primary and secondary educational institutions. At the municipal level, there are approximately 700 school districts statewide. The Ohio Board of Regents coordinates and assists with Ohio's institutions of higher education which have recently been reorganized into the University System of Ohio under Governor Strickland. The system averages an annual enrollment of over 400,000 students, making it one of the five largest state university systems in the U.S.
Ohio is home to some of the nation's highest-ranking public libraries.[120] The 2008 study by Thomas J. Hennen Jr. ranked Ohio as number one in a state-by-state comparison.[121] For 2008, 31 of Ohio's library systems were all ranked in the top ten for American cities of their population category.[120]
The Ohio Public Library Information Network (OPLIN) is an organization that provides Ohio residents with internet access to their 251 public libraries. OPLIN also provides Ohioans with free home access to high-quality, subscription research databases.
Ohio also offers the OhioLINK program, allowing Ohio's libraries (particularly those from colleges and universities) access to materials in other libraries. The program is largely successful in allowing researchers access to books and other media that might not otherwise be available.
Ohio is home to major professional sports teams in baseball, basketball, football, hockey, and soccer. The state's major professional sporting teams include: Cincinnati Reds (Major League Baseball),[122] Cleveland Indians (Major League Baseball),[123] Cincinnati Bengals (National Football League),[124] Cleveland Browns (National Football League),[124] Cleveland Cavaliers (National Basketball Association),[125] Columbus Blue Jackets (National Hockey League),[126] and the Columbus Crew (Major League Soccer).[127]
Ohio played a central role in the development of both Major League Baseball and the National Football League. Baseball's first fully professional team, the Cincinnati Red Stockings of 1869, were organized in Ohio.[128] An informal early 20th century American football association, the Ohio League, was the direct predecessor of the NFL, although neither of Ohio's modern NFL franchises trace their roots to an Ohio League club. The Pro Football Hall of Fame is located in Canton.
On a smaller scale, Ohio hosts minor league baseball, arena football, indoor football, mid-level hockey, and lower division soccer. The minor league baseball teams include: Akron Aeros (affiliated with the Cleveland Indians), Chillicothe Paints (independent), Columbus Clippers (affiliated with the Cleveland Indians), Dayton Dragons (affiliated with the Cincinnati Reds), Lake County Captains[129] (affiliated with the Cleveland Indians), Mahoning Valley Scrappers[130] (affiliated with the Cleveland Indians), and Toledo Mud Hens[131] (affiliated with the Detroit Tigers).
Ohio's minor professional football teams include: Canton Legends (American Indoor Football Association), Cincinnati Marshals (National Indoor Football League), Cincinnati Sizzle (National Women's Football Association), Cleveland Fusion (National Women's Football Association), Cleveland Gladiators (Arena Football League), Columbus Comets (National Women's Football Association), Columbus Destroyers (Arena Football League), Mahoning Valley Thunder (af2), Marion Mayhem (Continental Indoor Football League), and Miami Valley Silverbacks (Continental Indoor Football League).
Ohio's alternative professional hockey teams include: Cincinnati Cyclones (ECHL), Lake Erie Monsters (American Hockey League), Dayton Gems (Central Hockey League), Mahoning Valley Phantoms (North American Hockey League), Toledo Walleye (ECHL), and Youngstown Steelhounds (Central Hockey League).
In lower division professional soccer, Ohio accommodates the Cincinnati Kings and Cleveland City Stars, both of the United Soccer League and the Dayton Dutch Lions of the USL Premier Development League.
Ohio is also home to the Akron Racers, a minor professional softball club, of National Pro Fastpitch.
Former major league teams:
Ohio has eight NCAA Division I-A college football teams, divided among three different conferences. It has also experienced considerable success in the secondary and tertiary tiers of college football divisions.
In Division I-A, representing the Big Ten, the Ohio State Buckeyes football team ranks 5th among all-time winningest programs, with seven national championships and seven Heisman Trophy winners. Their biggest are rivals are the Michigan Wolverines, whom they traditionally play each year as the last game of their regular season schedule.
Ohio has six teams represented in the Mid-American Conference: the University of Akron, Bowling Green, Kent State, Miami University, Ohio University and the University of Toledo. The MAC headquarters are based in Cleveland.
The University of Cincinnati Bearcats represent Ohio in the Big East Conference.
Division I-AA Youngstown State is a perennial power in the Missouri Valley Football Conference, having won four FCS National Championships.
Division III Mount Union College boasts a record-setting ten National Championships and also hold the record for 110 consecutive game winning streak from 1994 until 2005. They have won two of the last three D-III National Championship games.
Ohio's state symbols:
Find more about Ohio on Wikipedia's sister projects: | |
Definitions and translations from Wiktionary |
|
Images and media from Commons |
|
Learning resources from Wikiversity |
|
News stories from Wikinews |
|
Quotations from Wikiquote |
|
Source texts from Wikisource |
|
Textbooks from Wikibooks |
Michigan • Lake Erie | ||||
Indiana | Pennsylvania | |||
Ohio: Outline • Index East | ||||
Kentucky • West Virginia |
|
|
|
Preceded by Tennessee |
List of U.S. states by date of statehood Admitted on March 1, 1803 (17th) |
Succeeded by Louisiana |
Coordinates: 40°30′N 82°30′W / 40.5°N 82.5°W / 40.5; -82.5
In geology, a valley or dale is a depression with predominant extent in one direction. A very deep river valley may be called a canyon or gorge.
The terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of these two main types or a mixture of them, (at least) with respect of the cross section of the slopes or hillsides.
Contents |
A valley in its broadest geographic sense is also known as a dale. A valley through which a river runs may also be referred to as a vale. A small, secluded, and often wooded valley is known as a dell or in Scotland as a glen. A wide, flat valley through which a river runs is known in Scotland as a strath. A mountain cove is a small valley, closed at one or both ends, in the central or southern Appalachian Mountains which sometimes results from the erosion of a geologic window. A small valley surrounded by mountains or ridges is sometimes known as a hollow. A deep, narrow valley is known as a coon (also spelled combe or coombe). Similar geological structures, such as canyons, ravines, gorges, gullies, and kloofs, are not usually referred to as valleys.
A valley formed by flowing water, or river valley, is usually V-shaped. The exact shape will depend on the characteristics of the stream flowing through it. Rivers with steep gradients, as in mountain ranges, produce steep walls and a bottom. Shallower slopes may produce broader and gentler valleys, but in the lowest stretch of a river, where it approaches its base level, it begins to deposit sediment and the valley bottom becomes a floodplain.
Some broad V examples are:
Some of the first human complex societies originated in river valleys, such as that of the Nile, Tigris-Euphrates, Indus, Ganges, Yangtze, Huang He, Mississippi, and arguably Amazon. In prehistory, the rivers were used as a source of freshwater and food (fish and game), as well as a place to wash and a sewer. The proximity of water moderated temperature extremes and provided a source for irrigation, stimulating the development of agriculture. Most of the first civilizations developed from these river valley communities.
In geography, a vale is a wide river valley, usually with a particularly wide flood plain or flat valley bottom. Vales commonly occur between the escarpment slopes of pairs of chalk downs, where the chalk dome has been eroded, exposing less resistant underlying rock, usually clay.
There are various forms of valley associated with glaciation that may be referred to as glacial valleys.
A valley carved by glaciers is normally U-shaped. The valley becomes visible upon the recession of the glacier that forms it. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice. Floor gradient does not affect the valley's shape, it is the glacier's size that does. Continuously flowing glaciers – especially in the ice age – and large-sized glaciers carve wide, deep incised valleys.
Examples of U-shaped valleys are found in every mountainous region that has experienced glaciation, usually during the Pleistocene ice ages. Most present U-shaped valleys started as V-shaped before glaciation. The glaciers carved it out wider and deeper, simultaneously changing the shape. This proceeds through the glacial erosion processes of glaciation and abrasion, which results in large rocky material (glacial till) being carried in the glacier. A material called boulder clay is deposited on the floor of the valley. As the ice melts and retreats, the valley is left with very steep sides and a wide, flat floor. A river or stream may remain in the valley. This replaces the original stream or river and is known as a misfit stream because it is smaller than one would expect given the size of its valley.
Other interesting glacially carved valleys include:
A tunnel valley is a large, long, U-shaped valley originally cut under the glacial ice near the margin of continental ice sheets such as that now covering Antarctica and formerly covering portions of all continents during past glacial ages.[1]
A tunnel valley can be up to 100 km (62 mi) long, 4 km (2.5 mi) wide, and 400 m (1,300 ft) deep (its depth may vary along its length).
Tunnel valleys were formed by subglacial erosion by water and served as subglacial drainage pathways carrying large volumes of melt water. Their cross-sections exhibit steep-sided flanks similar to fjord walls, and their flat bottoms are typical of subglacial glacial erosion.
In northern Central Europe, the Scandinavian ice sheet during the various ice ages advanced slightly uphill against the lie of the land. As a result its meltwaters flowed parallel to the ice margin to reach the North Sea basin, forming huge, flat valleys known as Urstromtäler. Unlike the other forms of glacial valley, these were formed by glacial meltwaters.
Depending on the topography, the rock types and the climate, a lot of transitional forms between V-, U- and plain valleys exist. Their bottoms can be broad or narrow, but characteristic is also the type of valley shoulder. The broader a mountain valley, the lower its shoulders are located in most cases. An important exception are canyons where the shoulder almost is near the top of the valley's slope. In the Alps – e.g. the Tyrolean Inn valley – the shoulders are quite low (100–200 meters above the bottom). Many villages are located here (esp. at the sunny side) because the climate is very mild: even in winter when the valley's floor is completely filled with fog, these villages are in sunshine.
In some stress-tectonic regions of the Rockies or the Alps (e.g. Salzburg) the side valleys are parallel to each other, and additionally they are hanging. The brooks flow into the river in form of deep canyons or waterfalls. Usually this fact is the result of a violent erosion of the former valley shoulders. A special genesis we find also at arêtes and glacial cirques, at every Scottish glen, or a northern fjord.
A hanging valley is a tributary valley with the floor at a higher relief than the main channel into which it flows. They are most commonly associated with U-shaped valleys when a tributary glacier flows into a glacier of larger volume. The main glacier erodes a deep U-shaped valley with nearly vertical sides while the tributary glacier, with a smaller volume of ice, makes a shallower U-shaped valley. Since the surfaces of the glaciers were originally at the same elevation, the shallower valley appears to be ‘hanging’ above the main valley. Often, waterfalls form at or near the outlet of the upper valley.[1] Hanging valleys are also the product of varying rates of erosion of the main valley and the tributary valleys. The varying rates of erosion are associated with the valleys rock composition of the adjacent rocks in the different valley locations. The tributary valleys are eroded and deepend by glaciers at a slower rate than that of the main valley floor. Thus the difference in the two valleys depth increases over time. The tributary valleys that were composed of more resistant rock then hangs over the main valley.[2]
Usually the bottom of a main valley is broad – independent of the U or V shape. It typically ranges from about one to ten kilometers in width and is commonly filled with mountain sediments. The shape of the floor can be rather horizontal, similar to a flat cylinder, or terraced.
Side valleys are rather V than U-shaped; near the mouth waterfalls are possible if it is a hanging valley. The location of the villages depends on the across-valley profile, on climate and local traditions, and on the danger of avalanches or landslides. Predominant are places on terraces or alluvial fans if they exist.
Historic siting of villages within the mainstem valleys, however, have chiefly considered the potential of flooding.
A hollow is a small valley or dry stream bed. This term is commonly used in New England, Appalachia, Arkansas and Missouri to describe such geographic features, in Appalachia it may be pronounced as "Holler". Hollows may be formed by river valleys such as Mansfield Hollow or they may be relatively dry clefts with a notch-like characteristic in that they have a height of land and consequent water divide in their bases.
Rift valleys, such as the Albertine Rift, are formed by the expansion of the Earth's crust due to tectonic activity beneath the Earth's surface.
Look up Valley in Wiktionary, the free dictionary. |
Wikimedia Commons has media related to: Valleys |
|