Cairo, Illinois in the context of "Ohio River"

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⭐ Core Definition: Cairo, Illinois

Cairo (/ˈkɛər/ KAIR-oh, sometimes /ˈkr/ KAY-roh) is the southernmost city in the U.S. state of Illinois and the county seat of Alexander County. A river city, Cairo has the lowest elevation of any location in Illinois and is the only Illinois city to be surrounded by levees. The city is named after Egypt's capital on the Nile and is located in the river-crossed area of Southern Illinois. It is coterminous with Cairo Precinct.

Cairo is located at the confluence of the Ohio and Mississippi rivers, the largest rivers in North America, and is near the Cache River complex, a Wetland of International Importance. Settlement began in earnest in the 1830s and busy river boat traffic expanded through the 1850s. Fort Defiance, a Civil War base, was located here in 1862 by Union General Ulysses S. Grant to control strategic access to the rivers and launch and supply his successful campaigns south. The town also served as a naval base for the Mississippi River Squadron to pursue the Anaconda Plan to win the war. Developed as a river port, Cairo was later bypassed by transportation changes away from the large expanse of low-lying land, wetland, and water, which surrounds Cairo and makes such infrastructure difficult, and due to industrial restructuring, the population peaked at 15,203 in 1920, while in the 2020 census it was 1,733.

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👉 Cairo, Illinois in the context of Ohio River

The Ohio River (Seneca: Ohi:yo') is a 981-mile-long (1,579 km) river in the United States. It is located at the boundary of the Midwestern and Southern United States, flowing in a southwesterly direction from Pittsburgh, Pennsylvania, to its mouth on the Mississippi River in Cairo, Illinois. It is the third largest river by discharge volume in the United States and the largest tributary by volume of the Mississippi River. It is also the sixth oldest river on the North American continent. The river flows through or along the border of six states, and its drainage basin includes parts of 14 states. Through its largest tributary, the Tennessee River, the basin includes several states of the southeastern United States. It is the source of drinking water for five million people.

The river became a primary transportation route for pioneers during the westward expansion of the early U.S. The lower Ohio River just below Louisville was obstructed by rapids known as the Falls of the Ohio where the elevation falls 26 feet (7.9 m) in 2 miles (3.2 km) restricting larger commercial navigation, although in the 18th and early 19th century its three deepest channels could be traversed by a wide variety of craft then in use. In 1830, the Louisville and Portland Canal (now the McAlpine Locks and Dam) bypassed the rapids, allowing even larger commercial and modern navigation from the Forks of the Ohio at Pittsburgh to the Port of New Orleans at the mouth of the Mississippi on the Gulf of Mexico. Since the "canalization" of the river in 1929, the Ohio has not been a natural free-flowing river; today, it is divided into 21 discrete pools or reservoirs by 20 locks and dams for navigation and power generation.

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Cairo, Illinois in the context of Mississippi River Valley

The Mississippi embayment is a physiographic feature in the south-central United States, part of the Mississippi Alluvial Plain. It is essentially a northward continuation of the fluvial sediments of the Mississippi River Delta to its confluence with the Ohio River at Cairo, Illinois. The current sedimentary area was formed in the Cretaceous and early Cenozoic by the filling with sediment of a pre-existing basin. An explanation for the embayment's formation was put forward by Van Arsdale and Cox in 2007: movement of the Earth's crust brought this region over a volcanic "hotspot" in the Earth's mantle causing an upthrust of magma which formed the Appalachian-Ouachita range. Subsequent erosion caused a deep trough that was flooded by the Gulf of Mexico and eventually filled with sediment from the Mississippi River.

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