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This page is about the river in the United States; for other uses, see Mississippi River (disambiguation).


The Mississippi River is the second-longest river in the United States; the longest is the Missouri River, which flows into the Mississippi. Taken together, they form the largest river system in North America. If measured from the head of the Missouri, the length of the Missouri/Mississippi combination is approximately 3,895 miles (6,270 km) long.

1 Geography


With its source Lake Itasca at 1475 feet above sea level in Itasca State Park in northern Minnesota, the river falls to 725 feet just below Saint Anthony Falls in Minneapolis. The Mississippi is joined by the Illinois River and the Missouri River at Saint Louis, and by the Ohio at Cairo, IllinoisCairo is a city located in Alexander County, Illinois. As of the 2000 census, the city had a total population of 3,632. It is the county seat of Alexander County. The city's name is pronounced differently from the English name for the Egyptian city of the.

The Mississippi drains most of the area between the Rocky MountainsThe Rocky Mountains often called the Rockies, are a broad mountain range in western North America. The Rocky Mountains stretch more than 3000 miles (4800 km) from Mexico, through the continental United States, into Canada and Alaska. The highest peak is M and the Appalachian MountainsThe Appalachian Mountains are a system of North American mountains running from Newfoundland and Labrador, Canada to Alabama in the United States, although the northernmost mainland portion ends at the Gaspe Peninsula of Quebec. The system is divided into, except for the area drained by the Great LakesThe Great Lakes are a group of five large lakes on or near the United States- Canadian border. They are the largest group of fresh water lakes in the world, and the Great Lakes-St. Lawrence system is the largest fresh-water system in the world. They are s. It runs through, or borders, ten states in the United States -- Minnesota, Wisconsin, Iowa, Illinois, Missouri, Kentucky, Arkansas, Tennessee, Mississippi and Louisiana -- before emptying into the Gulf of Mexico about 100 miles (160 km) downstream from New Orleans. A raindrop falling in Lake Itasca would arrive at the Gulf of Mexico in about 90 days. [1]


The river is divided into the upper Mississippi, from its source south to the Ohio River, and the lower Mississippi, from the Ohio to its mouth near New Orleans. The upper Mississippi is further divided into three sections: the headwaters, from the source to Saint Anthony Falls; a series of man-made lakes between Minneapolis and St. Louis; and the middle Mississippi, a relatively free-flowing river downstream of the confluence with the Missouri River at St. Louis.

A series of 27 locks and dams on the upper Mississippi, most of which were built in the 1930s, is designed primarily to maintain a nine-foot channel for commercial barge traffic. The lakes formed are also used for recreational boating and fishing. The dams make the river deeper and wider but do not stop it. No flood control is intended. During periods of high flow, the gates, some of which are submersible, are completely opened and the dams simply cease to function. Below St. Louis the Mississippi is relatively free-flowing, although it is constrained by numerous levees and directed by numerous wing dams.

The mouth of the Mississippi River has shifted repeatedly over time. Since a canal was built in the early nineteenth century, the river has been seeking the Atchafalaya River mouth, some 60 miles (95 km) from New Orleans. The U.S. Army Corps of Engineers maintains a massive system of locks to keep the river in its present course.

Other changes in the course of the river have occurred because of earthquakes along the New Madrid Fault Zone, which lies near the cities of Memphis and St. Louis. Three earthquakes in 1811 and 1812, estimated at approximately 8 on the Richter Scale, were said to have temporarily reversed the course of the Mississippi. These earthquakes also created Reelfoot Lake in Tennessee from the altered landscape near the river. The faulting is related to an aulacogen (geologic term for a failed rift) that formed at the same time as the Gulf of Mexico.

Davenport, Iowa is the only city over 20,000 people bordering the Mississippi that has no permanent floodwall or levee.

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