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Mississippi River

 
Dictionary: Mississippi River


The chief river of the United States, rising in the lake region of northern Minnesota and flowing about 3,781 km (2,350 mi) generally southward to enter the Gulf of Mexico through a huge delta in southeast Louisiana. Probably discovered by Hernando de Soto in 1541, it was explored by Jacques Marquette and Louis Jolliet in 1673. La Salle claimed the entire region for France after he descended to the river's mouth in 1682.

 

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Britannica Concise Encyclopedia: Mississippi River
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River, central U.S. It rises at Lake Itasca in Minnesota and flows south, meeting its major tributaries, the Missouri and the Ohio rivers, about halfway along its journey to the Gulf of Mexico. It enters the Gulf southeast of New Orleans, after a course of 2,350 mi (3,780 km). It is the largest river in North America, and with its tributaries it drains an area of 1.2 million sq mi (3.1 million sq km). Spanish explorer Hernando de Soto was the first European to discover the river in 1541. French explorers Louis Jolliet and Jacques Marquette traveled down it in 1673 as far as the Arkansas River. French explorer La Salle reached the delta in 1682 and claimed the entire Mississippi region for France, as Louisiana. France kept control over the upper river, but the lower portion passed to Spain in 1769. It was designated the western boundary of the U.S. in 1783. France sold it to the U.S. in 1803 as part of the Louisiana Purchase. During the American Civil War, Union forces captured Vicksburg, Miss., in 1863, breaking the Confederate hold on the river. As the central river artery of the U.S., it is one of the busiest commercial waterways in the world.

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

US History Encyclopedia: Mississippi River
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One of the major rivers of North America, the Mississippi River has been a focal point in American history, commerce, agriculture, literature, and environmental awareness. The length of the Mississippi River from its source in Lake Itasca in northwestern Minnesota to its mouth in the Gulf of Mexico flows 2,348 miles; it is the second longest river in the United States behind the Missouri (2,466 miles). The Mississippi River system drains the agricultural plains between the Appalachian Mountains to the east and the Rocky Mountains to the west. This drainage basin (approximately 1,234,700 square miles) covers about 40 percent of the United States and ranks as the fifth largest in the world.

Mississippi River's Course

The Mississippi River actually begins as a small stream flowing from Lake Itasca, Minnesota. The river initially flows north and then east as the means of connecting several lakes in northern Minnesota. The river begins to flow southward near Grand Rapids, Minnesota, and is joined with the Minnesota River between the cities of Minneapolis and Saint Paul. The muddy waters of the Missouri River flow into the clear waters of the Mississippi River just north of St. Louis, Missouri. At this point, the Mississippi becomes brown and muddy for the rest of the journey south.

At Cairo, Illinois, the Ohio River flows into the Mississippi, doubling its volume and creating the point that divides the Upper Mississippi from the Lower Mississippi. The Lower Mississippi Valley is a wide and fertile region. In this area, the river meanders its way south and over time has continuously changed its course, leaving behind numerous oxbow lakes as remnants of its past. As it flows in this southern region, the Mississippi deposits rich silt along its banks. In many areas, the silt builds up to create natural levees. South of Memphis, Tennessee, the Arkansas River junctions with the Mississippi River. Near Fort Adams, Mississippi, the Red River joins with the Mississippi, diverting with it about a quarter of the flow of the Mississippi into the Atchafalaya River.

As the Mississippi River nears the Gulf of Mexico it creates a large delta with its silt. The Mississippi River delta covers approximately 13,000 square miles. South of the city of New Orleans, the Mississippi creates several channels, known as distributaries, which then flow separately into the Gulf of Mexico. The most prominent of these are known as the North Pass, South Pass, Southwest Pass, and Main Pass. Annually, the Mississippi River discharges about 133 cubic miles of water (approximately 640,000 cubic feet per second).

History

The Mississippi River played an important role in the lives of many Native Americans who lived in the Upper Mississippi Valley, such as the Santee Dakota, the Illinois, the Kickapoo, and the Ojibwe, as well as those tribes in the southern valley, such as the Chicksaw, the Choctaw, the Tunica, and the Natchez. The name "Mississippi," meaning "great river" or "gathering of water," is attributed to the Ojibwe (Chippewa).

The first known European to travel on the Mississippi River was the Spaniard Hernando de Soto, who crossed the river near present-day Memphis in May 1541. Over a century later, in 1673, the French explorers Louis Jolliet and Father Jacques Marquette entered the Mississippi River from the Wisconsin River and traveled by canoe downriver to a point near the mouth of the Arkansas River. Less than a decade later, another Frenchman, René-Robert Cavelier, Sieur de La Salle, explored the Mississippi River from the Illinois River to the Gulf of Mexico. La Salle declared on 9 April 1682 that the Mississippi Valley belonged to France, and he named the region Louisiana. It was not until 1718 that the French were actually established at New Orleans. They maintained control over the lower Mississippi until the end of the French and Indian War (1754–1763). In 1762 and 1763, the French made cessions that established the Mississippi River as an international boundary with Spanish territory to the west and British territory to the east.

During the American Revolution (1775–1783), the river served as the supply line for George Rogers Clark, allowing him to maintain control of the Illinois country. The Peace of Paris of 1783 outlined the new country of the United States as extending to the Mississippi River between Spanish Florida and the Canadian border. Additionally, the United States was entitled to free navigation of the Mississippi River. Spain, though not party to the treaty, controlled the mouth of the Mississippi and, through high duties, maintained actual power over the river and, in essence, over the entire Mississippi Valley. Not until Pinckney's Treaty with Spain in 1795 was the river truly free to American navigation. This freedom was short-lived, however, for when Spain ceded Louisiana back to France in 1800, the French again closed the Mississippi to American river traffic. Finally, the Louisiana Purchase (1803) made the Mississippi an American river, and it rapidly became a major route of trade and commerce for the entire Mississippi Valley.

Western settlers and traders traversed the Mississippi in flatboats (on which farmers floated their produce downstream to market) and keelboats (which could be pushed upstream with great effort). Certainly the most significant change in river transportation on the Mississippi came in 1811 when the steamboat New Orleans made its legendary trip from Pittsburgh to New Orleans. This event opened the Mississippi River to two-way traffic, essentially doubling the carrying capacity of the river. By 1860, more than 1,000 steamboats were actively engaged in transport along the Mississippi River system, and the cities of Cincinnati (Ohio), Louisville, (Kentucky), St. Louis, Memphis, and New Orleans became important cities in the movement west.

During the Civil War (1861–1865) both the Union and the Confederacy recognized the importance of the Mississippi River, and the fight over its control was a major part of the war. A decisive victory for the Union came with the fall of Vicksburg, Mississippi (1863), which essentially gave the Union full possession of the river, reopening the trade routes down the Mississippi from the Ohio Valley and splitting the Confederacy.

Following the war, life on the Mississippi did not return to the golden years so richly described in Mark Twain's writings. The faster and more convenient railroads replaced much of the commercial traffic on the Mississippi. In 1879, the U.S. Congress established the Mississippi River Commission as a means of maintaining and improving the river as a commercial waterway. In the years that followed, the commission deepened and widened several channels along the river, making it more navigable for larger boats and barges. These changes promoted increased transport on the Mississippi, particularly of heavy and bulky freight.

At the turn of the twenty-first century, the Mississippi River carried more than half of the freight transported on American inland water. Nearly 460 million short tons of freight were transported on the Mississippi River each year. Most of this freight was carried on large barges pushed by tugboats. The upper Mississippi traffic was predominantly composed of agricultural products such as wheat, corn, and soybeans. Coal and steel freight traveled down the Ohio River and onto the lower Mississippi River. At Baton Rouge, Louisiana, petroleum, petrochemical products, and aluminum joined the freight being moved south. It is at this point that the depth of the Mississippi River increases, allowing for larger ships to traverse upriver to this point.

Flooding

People living along the Mississippi River are well aware of the flooding potential of the river. During de Soto's exploration of the Mississippi, he noted much flooding. Evidence from Native American Mississippi Valley settlement locations (on higher land) and the creation of mounds on which they placed their dwellings indicate Native American awareness of and adaptation to flooding of the Mississippi. Significant flooding of the Mississippi Valley in 1927 prompted national discussion of flood control along the Mississippi. Other severe flooding events occurred in 1937, 1965, 1973, 1982, and 1993. The severe flooding in 1993 is considered to be the most devastating in recorded U.S. history. It affected the upper and middle Mississippi Valley from late June until mid-August 1993 with record levels on the Mississippi River and most of its tributaries from Minnesota to Missouri. At St. Louis, the river remained above flood stage for over two months and crested at 49.6 feet (19 feet above flood stage). Industry and transportation along the Mississippi were virtually at a standstill during the summer months of 1993. In all, over 1,000 of the 1,300 levees in the Mississippi River system failed, over 70,000 people were displaced, nearly 50,000 homes were either destroyed or damaged, 12,000 square miles of agricultural land was unable to be farmed, and 52 people died. Fortunately, larger cities along the Mississippi remained protected by floodwalls. The cost of the flood was enormous. Most estimates of total flood damage run to nearly $20 billion. Flood events are certain to remain a part of life along the Mississippi River.

Human Influence

Humans have influenced the flow of the Mississippi and the quality of its water. Historically, the river and its tributaries meandered across the floodplain, and erosion, sedimentation, and flooding were natural processes. During the twentieth century, however, humans interrupted these processes. In the 1930s, twenty-nine navigation dams were built between St. Louis and Minneapolis. These dams impound the water to improve navigation. One cost of damming, however, is increased retention of sediment in the river. Flood-control levees have been built in order to manage the seasonal flooding. Much of the Mississippi floodplain has been converted to agriculture. This change has two serious consequences for the Mississippi River. First, the loss of prairie wetlands and floodplain forest decreases the biodiversity of the region. Second, conversion of land to agriculture often leads to increased run off of fertilizers and pesticides. The presence of high rates of nitrogen and phosphorus can be directly attributed to farming practices in the Mississippi Valley. At the end of the twentieth century, many experts suggested that agricultural pollution in the Mississippi River was directly responsible for the creation of the "dead zone," an area in the Gulf of Mexico where there is little aquatic life due to abnormally low levels of oxygen.

Industrial pollution is also a concern along the Mississippi River. Industries have contributed significant amounts of oil, aluminum, lead, and other industrial wastes such as sulfur dioxide, hydrogen sulfide, and benzene to the flow of the Mississippi. A study in 2000 estimated that 58 million pounds of toxic discharge travels down the Mississippi annually. At the turn of the twenty-first century, much of the river remained unswimmable and unfishable, despite the fact that it serves as the primary source of drinking water for 18 million people. Growing awareness of environmental processes and increased concern for the state of the Mississippi River system that began during the last decade of the twentieth century may prove to have a positive influence in the life of the great river.

Bibliography

Badt, Karin. The Mississippi Flood of 1993. Chicago: Children's Press, 1994.

Geus, Theodor. The Mississippi. Lexington: University Press of Kentucky, 1989.

Haites, Erik, James Mak, and Gary Walton. Western River Transportation: The Era of Early Internal Development, 1810–1860. Baltimore: Johns Hopkins University Press, 1975.

Lauber, Patricia. Flood: Wrestling with the Mississippi. Washington, D.C.: National Geographic Society, 1996.

 
Columbia Encyclopedia: Mississippi
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Mississippi, river, principal river of the United States, c.2,350 mi (3,780 km) long, exceeded in length only by the Missouri River, the chief of its numerous tributaries. The combined Missouri-Mississippi system (from the Missouri's headwaters in the Rocky Mts. to the mouth of the Mississippi River) is c.3,740 mi (6,020 km) long and ranks as the world's third longest river system after the Nile and the Amazon. With its tributaries, the Mississippi drains c.1,231,000 sq mi (3,188,290 sq km) of the central United States, including all or part of 31 states and c.13,000 sq mi (33,670 sq km) of Alberta and Saskatchewan in Canada. Cotton and rice are important crops in the lower Mississippi valley; sugarcane is raised in the delta. The Mississippi is abundant in freshwater fish; shrimp are taken from the briny delta waters. The delta also yields sulfur, oil, and gas.

Course and Navigation

The Mississippi River rises in small streams that feed Lake Itasca (alt. 1,463 ft/446 m) in N Minnesota and flows generally south to enter the Gulf of Mexico through a huge delta in SE Louisiana. A major economic waterway, the river is navigable from the sediment-free channel maintained through South Pass in the delta to the Falls of St. Anthony in Minneapolis, with canals circumventing the rapids near Rock Island, Ill., and Keokuk, Iowa. For the low-water months of July, August, and September, there is a 45-ft (13.7-m) channel navigable by oceangoing vessels from Head of the Passes to Baton Rouge, La., and a 9-ft (2.7-m) channel from Baton Rouge deep enough for barges and towboats to Minneapolis. The Mississippi connects with the Intracoastal Waterway in the south and with the Great Lakes-St. Lawrence Seaway system in the north by way of the Illinois Waterway.

Along the river's upper course shipping is interrupted by ice from December to March; thick, hazardous fogs frequently settle on the cold waters of the unfrozen sections during warm spells from December to May. In its upper course the river is controlled by numerous dams and falls c.700 ft (210 m) in the 513-mi (826-km) stretch from Lake Itasca to Minneapolis and then falls c.490 ft (150 m) in 856 mi (1,378 km) from Minneapolis to Cairo, Ill. The Mississippi River receives the Missouri River 17 mi (27 km) N of St. Louis and expands to a width of c.3,500 ft (1,070 m); it swells to c.4,500 ft (1,370 m) at Cairo, where it receives the Ohio River.

The lower Mississippi meanders in great loops across a broad alluvial plain (25-125 mi/40-201 km wide) that stretches from Cape Girardeau, Mo., to the delta region S of Natchez, Miss. The plain is marked with oxbow lakes and marshes that are remnants of the river's former channels. Natural levees, built up from sediment carried and deposited in times of flood, border the river for much of its length; sediment has also been deposited on the riverbed, so that in places the surface of the Mississippi is above that of the surrounding plain, as evidenced by the St. Francis, Black, Yazoo, and Tensas river basins. Breaks in the levees frequently flood the fertile bottomlands of these and other low-lying areas of the plain.

The Mississippi Delta

After receiving the Arkansas and Red rivers, the Mississippi enters a birdsfoot-type delta, which was built outward by sediment carried by the main stream since c.A.D. 1500 It then discharges into the Gulf of Mexico through a number of distributaries, the most important being the Atchafalaya River and Bayou Lafourche. The main stream continues southeast through the delta to enter the gulf through several mouths, including Southeast Pass, South Pass, and Pass à Loutre. Indications that the Mississippi River might abandon this course and divert through the Atchafalaya River led to the construction of a series of dams, locks, and canals by the U.S. Army Corps of Engineers. Known as the Old River Control Structure, it was undertaken to prevent such an occurrence. Sluggish bayous and freshwater lakes (such as Pontchartrain, Grand, and Salvador) dot the delta region.

Regarding the delta, environmentalists and those in the seafood industry are concerned by the loss of 25-45 sq mi (65-104 sq km) of marsh a year; fish and wildlife populations are threatened as their natural habitat slowly disappears. The loss has been attributed to subsidence and a decrease in sediment largely due to dams, artificial channeling, and land conservation measures. Pollution and the cutting of new waterways for petroleum exploration and drilling have also taken their toll on the delta. Louisiana has enacted environmental protection laws that are expected to slow, but not halt, the loss of the delta marshes.

Attempts at Flood Control

The flow of the river is greatest in the spring, when heavy rainfall and melting snow on the tributaries (especially the Missouri and the Ohio) cause the main stream to rise and frequently overflow its banks and levees, inundating vast areas of the plain. Since the disastrous flood of 1927 the U.S. Congress has authorized the construction of dams on the upper Mississippi and its tributaries to regulate the flow; the building of c.1,600 mi (2,580 km) of levees below Cape Girardeau to contain the swollen river; and the establishment of floodways to divert water at critical points, such as the Cairo-New Madrid, Atchafalaya, and Morganza floodways and the Bonnet Carre Spillway at New Orleans, which diverts water into Lake Pontchartrain. Cutoffs have eliminated the dangerous winding channels, and an improved main channel has increased the river's flood-carrying capacity. A 220-acre (89-hectare) model of the Mississippi River basin is located at Clinton, Miss., which has been used by the U.S. Corps of Engineers to simulate various conditions in the basin.

Nonetheless, serious, record-breaking floods again occurred in the rainy spring of 1973, when the river crested at St. Louis at 43.3 ft (13.2 m), and again in the summer of 1993, when the river crested at St. Louis at 49.6 ft (15.1 m), killing 50 people, displacing 50,000, and causing $12 billion in agricultural and property damage. The narrow river channel that has been created by building levees has worsened flooding in some instances. In 1988 a severe drought brought water levels down to their lowest point in recorded history and halted most river traffic.

History

The Spanish explorer Hernando De Soto is credited with the European discovery of the Mississippi River in 1541. The French explorers Jacques Marquette and Louis Jolliet reached it through the Wisconsin River in 1673, and in 1682 La Salle traveled down the river to the Gulf of Mexico and claimed the entire territory for France. The French founded New Orleans in 1718 and effectively extended control over the upper river basin with settlements at Cahokia, Kaskaskia, Prairie du Chien, and St. Louis. France ceded the river to Spain in 1763 but regained it in 1800; the United States acquired the Mississippi River as part of the Louisiana Purchase in 1803.

A major artery for the Native Americans and the fur-trading French, the river became in the 19th cent. the principal outlet for the newly settled areas of mid-America; exports were floated downstream with the current, and imports were poled or dragged upstream on rafts and keelboats. The first steamboat plied the river in 1811, and successors became increasingly luxurious as river trade increased in profitability and importance; the era is colorfully described in Mark Twain's Life on the Mississippi (1883).

Traffic from the north ceased after the outbreak of the Civil War. During the Civil War the Mississippi was an invasion route for Union armies and the scene of many important battles. Especially decisive were the capture of New Orleans (1862) by Adm. David Farragut, the Union naval commander, and the victory of Union forces under Grant at Vicksburg in 1863. River traffic resumed after the war, but much of the trade was lost to the railroads. With modern improvements in the channels of the river there has been a great increase in traffic, especially since the mid-1950s, with principal freight items being petroleum products, chemicals, sand, gravel, and limestone.

Bibliography

See B. Keating, The Mighty Mississippi (1971); P. V. Scarpino, Great River: An Environmental History of the Upper Mississippi (1985); M. M. Smart et al., ed., Ecological Perspectives of the Upper Mississippi River (1986); J. M. Barry, Rising Tide: The Great Mississippi Flood of 1927 and How It Changed America (1997).


Geography: Mississippi River
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The longest river in the United States, flowing over two thousand miles from Minnesota to Louisiana and into the Gulf of Mexico.

Wikipedia: Mississippi River
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Mississippi River
River
Aerial view of Lock and Dam 12 on the Mississippi River at Bellevue, Iowa
Country  United States
States Minnesota, Wisconsin, Iowa, Illinois, Missouri, Kentucky, Tennessee, Arkansas, Mississippi, Louisiana
Tributaries
 - left St. Croix River, Illinois River, Rock River, Ohio River
 - right Minnesota River, Missouri River, White River, Arkansas River, Red River
Cities Minneapolis, MN, St. Paul, MN, St. Louis, MO, Memphis, TN, Baton Rouge, LA, New Orleans, LA
Source Lake Itasca[1]
 - location Itasca State Park, Clearwater County, MN
 - elevation 1,475 ft (450 m)
 - coordinates 47°14′23″N 95°12′27″W / 47.23972°N 95.2075°W / 47.23972; -95.2075
Mouth Gulf of Mexico
 - location Pilottown, Plaquemines Parish, LA
 - elevation ft (0 m)
 - coordinates 29°09′13″N 89°15′03″W / 29.15361°N 89.25083°W / 29.15361; -89.25083
Length 2,320 mi (3,734 km)
Basin 1,151,000 sq mi (2,981,076 km2)
Discharge for Baton Rouge, LA
 - average 450,000 cu ft/s (12,743 m3/s) [2]
Map of the Mississippi River

The Mississippi River is the largest river system in the United States and also the largest of North America.[3][4] About 2,320 miles (3,730 km) long,[5] the river originates at Lake Itasca, Minnesota and flows slowly southwards in sweeping meanders, terminating 95 river miles below New Orleans, Louisiana where it begins to flow to the Gulf of Mexico. Along with its major tributary, the Missouri River, the river drains all or parts of 31 U.S. states stretching from the Rocky Mountains in the west to the Appalachian Mountains in the east to the Canada-U.S. border on the north, including most of the Great Plains, and is the fourth longest river in the world and the tenth most powerful river in the world.

The current form of the Mississippi River basin was largely shaped by the Cordilleran Ice Sheet of the most recent Ice Age. The southernmost extent of this enormous glaciation extended well into the present-day United States and Mississippi basin. When the ice sheet began to recede, hundreds of feet of rich sediment were deposited, creating the flat and fertile landscape of the Mississippi Valley. During the melt, giant glacial rivers found drainage paths into the Mississippi watershed, creating such features as the Minnesota River, James River, and Milk River valleys. When the ice sheet completely retreated, many of these "temporary" rivers found paths to Hudson Bay or the Arctic Ocean, leaving the Mississippi Basin with many features "oversized" for the existing rivers to have carved in the same time period. The Mississippi River Delta has shifted and changed constantly since the formation of the river, but the construction of dams on the river has greatly reduced the flow of sediment to the delta. In recent years, the Mississippi's mouth has shown a steady shift towards the Atchafalaya River channel, but because of floodworks at the river's mouth, this change of course—which would be catastrophic for seaports at the river mouth—has been held at bay.

Hundreds of Native American tribes have depended on the Mississippi River and its tributaries for thousands of years. Although they knew the river by a melange of different names, it was the Ojibwe word misi-ziibi, meaning Great River, or gichi-ziibi, or Big River, that ultimately gave the river its present-day name. European explorers reached the mouth of the river as early as the 1500s and 1600s. The river throughout history has served as the border for New France, New Spain, and the early United States—its size and importance made it a formidable boundary as well as a strategic military location, and later, an important artery for steamboats to travel on. Writer Mark Twain was one of the most well-known figures on the river in this period. Even today, the river serves as partial boundaries for ten states, and most of its course can easily be seen on a political map. The Mississippi has also been known for great flooding events, especially in the twentieth century which experienced up to four 100-year floods. This has led to the construction of hundreds of miles of levees along nearly the entire course of the river, although they have not always succeeded to prevent the greatest floods.

Throughout its history, whether for Native Americans, explorers, or modern commerce, the Mississippi has always been a major navigation route through the center of North America. In the 19th and 20th centuries, despite its slow current and relative depth, a series of dams were constructed on the river, one of the most notable of which is at St. Anthony Falls on the border between Minneapolis and St. Paul. These dams facilitate navigation for a steady stream of barge traffic carrying agricultural products from the fertile Mississippi Basin to the Gulf Coast, and like the Columbia River, most of the Mississippi also is a cascade of reservoirs. Most of its big tributaries—the Missouri and Ohio Rivers—have also been developed for navigation. However, the development of the 20th and 21st centuries has also come with environmental problems, the most infamous of which is the enormous Gulf of Mexico dead zone that extends hundreds of miles out to sea from the river's mouth. Because of dredging activity to deepen the Mississippi River channel, many natural features such as sandbars and meanders no longer exist. Efforts are being made to clean up the river and its tributaries, including the establishment of National Park Service sites on the river and the prevention of agricultural waste from flowing into the river.

Contents

Geography

Confluence of the Mississippi and Ohio Rivers at Cairo, Illinois (2006)

From its origin at Lake Itasca to St. Louis, Missouri, the flow of the Mississippi River is moderated by 43 dams. Fourteen of these dams are located above Minneapolis, Minnesota in the headwaters region and serve multiple purposes including power generation and recreation. The remaining 29 dams beginning in downtown Minneapolis all contain locks and were constructed to permit commercial navigation of the upper river. Taken as a whole these 43 dams significantly shape the geography and influence the ecology of the upper river. Beginning just below Saint Paul, Minnesota and continuing throughout the upper and lower river, the Mississippi is further controlled by thousands of wing dikes that moderate the river's flow in order to maintain an open navigation channel and prevent the river from eroding its banks.

The Mississippi River runs through 10 states and was used to define portions of these states' borders. The middle of the riverbed at the time the borders were established was the line to define the borders between states.[6][7] The river has since shifted, but the state borders of Wisconsin, Iowa, Illinois, Missouri, Kentucky, Arkansas, Tennessee, and Mississippi have not changed; they still follow the former bed of the Mississippi River as of their establishment.

The widest point of the Mississippi River is Lake Winnibigoshish, near Grand Rapids, Minnesota, at over 7 miles (11 km) across. Also of note is Lake Onalaska, near La Crosse, Wisconsin, where the river is over 4 miles (6.4 km) wide (created by Lock and Dam No. 7) and Lake Pepin at more than 2 miles (3.2 km) wide.[8] However, the first two areas are lakes or reservoirs rather than free flowing water. In other areas where the Mississippi is a flowing river (other than Lake Pepin), it exceeds 1 mile (1.6 km) in width in several places in its lower course.

The Missouri River flows from the confluence of the Jefferson, Madison and Gallatin Rivers and is the longest river in the United States.[4] Taken together, the Jefferson, the Missouri, and the Mississippi form the longest river system in North America. If measured from the source of the Jefferson at Brower's Spring, to the Gulf of Mexico, the length of the Mississippi-Missouri-Jefferson combination is approximately 3,900 miles (6,300 km), making the combination the 4th longest river in the world. The uppermost 207 miles (333 km) of this combined river are called the Jefferson, the lowest 1,352 miles (2,176 km) are part of the Mississippi, and the intervening 2,341 miles (3,767 km) are called the Missouri.

The Arkansas River is the second-longest tributary of the Mississippi River. Measured by water volume, the largest of all Mississippi tributaries is the Ohio River.

The Mississippi 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.

Upper Mississippi River

The beginning of the Mississippi River at Lake Itasca (2004)

The upper Mississippi River is divided into three sections: the headwaters, 493 miles (793 km); from the source to Saint Anthony Falls; a series of man-made lakes between Minneapolis and St. Louis, Missouri, 664 miles (1,069 km); and the middle Mississippi, 190 miles (310 km), a relatively free-flowing river downstream of the confluence with the Missouri River at St. Louis.

Source

The source of the Upper Mississippi River is Lake Itasca, 1,475 feet (450 m) above sea level in Itasca State Park located in Clearwater County, Minnesota. The name "Itasca" is a combination of the last four letters of the Latin word for truth (veritas) and the first two letters of the Latin word for head (caput).

The uppermost lock and dam on the Mississippi River is the Upper St. Anthony Falls Lock and Dam in Minneapolis. Above the dam, the river's elevation is 799 feet (244 m). Below the dam, the river's elevation is 750 feet (230 m). This 49-foot (15 m) drop is the largest of all the Mississippi River locks and dams. The origin of the dramatic drop is a waterfall preserved adjacent to the lock under an apron of concrete. Saint Anthony Falls is the only true waterfall on the entire Mississippi River. The water elevation continues to drop steeply as it passes through the gorge carved by the waterfall. By the time the river reaches Saint Paul, Minnesota, below Lock and Dam #1, it has dropped more than half its original elevation and is 687 feet (209 m) above sea level. From St. Paul to St. Louis Missouri the river elevation falls much more slowly and is controlled and managed as a series of pools created by 26 locks and dams.[9] From St. Louis to the Ohio River confluence, the Mississippi free falls a total of 220 feet (67 m) over a distance of 180 miles (290 km) for an average rate of 1.2 feet per mile (23 cm/km). At the Ohio River confluence the Mississippi is 315 feet (96 m) above sea level.

Tributaries

The Mississippi is joined by the Minnesota River south of the Twin Cities, the St. Croix River near Prescott, Wisconsin, the Black River (Mississippi River), La Crosse River, and Root River (Minnesota) in La Crosse, Wisconsin the Wisconsin River in Prairie du Chien, Wisconsin, the Rock River in the Quad Cities, the Iowa River near Wapello, Iowa, the Skunk River south of Burlington, Iowa, the Des Moines River in Keokuk, Iowa, the Illinois River and the Missouri River near St. Louis, and by the Ohio River at Cairo, Illinois.

Lower Mississippi River

Major sub-tributaries include the Tennessee River (a tributary of the Ohio River) and the Platte River (a tributary of the Missouri River). The Arkansas River joins the Mississippi in southeastern Arkansas. The Yazoo River meets the Mississippi at Vicksburg. The Atchafalaya River in Louisiana is a major distributary of the Mississippi.

Communities along the river

In Minnesota, the Mississippi River runs through the Twin Cities (2007)
Community of boathouses on the Mississippi River in Winona, MN (2006)
The Mississippi River just north of St. Louis (2005)

Many of the communities along the Mississippi River are listed below. They have either historic significance or cultural lore connecting them to the river. They are ordered from the beginning of the river to its end.

Bridge crossings

The Chain of Rocks Bridge at St.Louis, Missouri

The first bridge across the Mississippi River was built in 1855. It spanned the river in Minneapolis where the current Hennepin Avenue Bridge is located.[10]

The first railroad bridge across the Mississippi was built in 1856. It spanned the river between the Rock Island Arsenal and Davenport, Iowa. Steamboat captains of the day, fearful of competition from the railroads, considered the new bridge "a hazard to navigation". Two weeks after the bridge opened, the steamboat Effie Afton rammed part of the bridge and started it on fire. Legal proceedings ensued, with Abraham Lincoln defending the railroad. The lawsuit went to the Supreme Court of the United States and was eventually ruled in favor of the railroad.

Below is a general overview of bridges over the Mississippi which have notable engineering or landmark significance with its city. They are ordered from the source to the mouth.

Watershed

Mississippi watershed (2005)

The Mississippi River has the third largest drainage basin or "catchment" in the world. The basin covers more than 1,245,000 sq mi (3,220,000 km2), including all or parts of 31 states and two Canadian provinces. The drainage basin empties into the Gulf of Mexico.

Major tributaries of the Mississippi:

Sequence of NASA MODIS images showing the outflow of fresh water from the Mississippi (arrows) into the Gulf of Mexico (2004)

Drainage area and basin

The Mississippi River drains the majority of the area between the Rocky Mountains and the Appalachian Mountains, except for the areas drained to the Hudson Bay via the Red River of the North, by the Saint Lawrence River and the Great Lakes, the Rio Grande (and numerous other rivers in Texas), the Alabama River-Tombigbee River, and the Chattahoochee River-Apalachicola River.

The Mississippi River empties into the Gulf of Mexico about 100 miles (160 km) downstream from New Orleans. Measurements of the length of the Mississippi from Lake Itasca to the Gulf of Mexico vary somewhat, but the United States Geological Survey's number is 2,340 miles (3,770 km). The retention time from Lake Itasca to the Gulf is about 90 days.[11]

Outflow

Fresh river water flowing from the Mississippi into the Gulf of Mexico does not mix into the salt water immediately. The images from NASA's MODIS to the right show a large plume of fresh water, which appears as a dark ribbon against the lighter-blue surrounding waters.

The images demonstrate that the plume did not mix with the surrounding sea water immediately. Instead, it stayed intact as it flowed through the Gulf of Mexico, into the Straits of Florida, and entered the Gulf Stream. The Mississippi River water rounded the tip of Florida and traveled up the southeast coast to the latitude of Georgia before finally mixing in so thoroughly with the ocean that it could no longer be detected by MODIS.

Discharge

The Mississippi river discharges at an annual average rate of between 200 and 700 thousand cubic feet per second (7,000–20,000 m3/s).[12] Although it is the 5th largest river in the world by volume, this flow is a mere fraction of the output of the Amazon, which moves nearly 7 million cubic feet per second (200,000 m3/s) during wet seasons. On average, the Mississippi has only 9% the flow of the Amazon River, but is nearly twice that of the Columbia River and almost 6 times the volume of the Colorado River.

History

View along the former riverbed at the TN/AR state line near Reverie, TN (2007)

Course changes

Ice sheets during the Illinoian Stage about 300,000 to 132,000 years before present, blocked the Mississippi near Rock Island, Illinois, diverting it to its present channel farther to the west, the current western border of Illinois.

The Hennepin Canal roughly follows the ancient channel of the Mississippi downstream from Rock Island to Hennepin. South of Hennepin, Illinois, the current Illinois River is actually following the ancient channel of the Mississippi River to Alton, Illinois, before the Illinoian Stage.

Other changes in the course of the river have occurred because of earthquakes along the New Madrid Seismic Zone, which lies between Memphis and St. Louis. Three earthquakes in 1811 and 1812, estimated at approximately 8 on the Richter magnitude scale, were said to have temporarily reversed the course of the Mississippi. The settlement of Reverie, Tennessee was cut off from Tipton County, Tennessee, during the 1811 and 1812 earthquakes and placed on the western side of the Mississippi River, the Arkansas side. 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.

Through a natural process known as delta switching, the lower Mississippi River has shifted its final course to the mouth of the Gulf of Mexico every thousand years or so. This occurs because the deposits of silt and sediment begin to clog its channel, raising the river's level and causing it to eventually find a steeper, more direct route to the Gulf of Mexico. The abandoned distributaries diminish in volume and form what are known as bayous. This process has, over the past 5,000 years, caused the coastline of south Louisiana to advance toward the Gulf from 15 to 50 miles (25–80 km). The currently active delta lobe is called the Birdfoot Delta, after its shape, or the Balize Delta, after La Balize, Louisiana, the first French settlement at the mouth of the Mississippi.

Native Americans

The area of the Mississippi valley was first settled by Native American tribes, such as the Cheyenne, Sioux, Ojibwe, Potawatomi, Ho-Chunk, Fox, Kickapoo, Tamaroa, Moingwena, Quapaw and Chickasaw.

The Cheyenne, one of the earliest inhabitants of the upper Mississippi River, called it the Máˀxe-éˀometaaˀe (Big Greasy River) in the Cheyenne language. However, the word Mississippi comes from Messipi, the French rendering of the Anishinaabe (Ojibwe or Algonquin) name for the river, Misi-ziibi (Great River).[13][14]

The Ojibwe called Lake Itasca Omashkoozo-zaaga'igan (Elk Lake) and the river flowing out of it Omashkoozo-ziibi (Elk River). After flowing into Lake Bemidji, the Ojibwe called the river Bemijigamaag-ziibi (River from the Traversing Lake). After flowing into Cass Lake, the name of the river changes to Gaa-miskwaawaakokaag-ziibi (Red Cedar River) and then out of Lake Winnibigoshish as Wiinibiigoozhish-ziibi (Miserable Wretched Dirty Water River), Gichi-ziibi (Big River) after the confluence with the Leech Lake River, then finally as Misi-ziibi (Great River) after the confluence with the Crow Wing River.[15] After the expeditions by Giacomo Beltrami and Henry Schoolcraft, the longest stream above the juncture of the Crow Wing River and Gichi-ziibi was named "Mississippi River". The Mississippi River Band of Chippewa Indians, known as the Gichi-ziibiwininiwag, are named after the stretch of the Mississippi River known as the Gichi-ziibi.

Discovery of the Mississippi by De Soto A.D. 1541 (1847–53) by William Henry Powell depicts DeSoto seeing the River for the first time.

European exploration

On May 8, 1541, Spanish explorer Hernando de Soto became the first recorded European to reach the Mississippi River, which he called Río del Espíritu Santo ("River of the Holy Spirit"), in the area of what is now Mississippi. In Spanish, the river is called Río Mississippi.[16]

French explorers, Louis Jolliet and Jacques Marquette, began exploring the Mississippi in the 17th century. Marquette traveled with a Sioux named Ne Tongo ("Big river" in Sioux language) in 1673. Marquette proposed calling it the River of the Immaculate Conception.

In 1682, René-Robert Cavelier, Sieur de La Salle and Henri de Tonti claimed the entire Mississippi River Valley for France, calling the river Colbert River after Jean-Baptiste Colbert and the region La Louisiane, for King Louis XIV. On March 2, 1699, Pierre Le Moyne d'Iberville rediscovered the mouth of the Mississippi, following the death of La Salle.[17] The French built the small fort of La Balise there to control passage.

In 1718, about 100 miles (160 km) upriver, New Orleans was established along the river crescent by Jean-Baptiste Le Moyne, Sieur de Bienville, with construction patterned after the 1711 resettlement on Mobile Bay of Mobile, the capital of French Louisiana at the time.

18th century

Following Britain's victory in the Seven Years War the Mississippi became the border between the British and Spanish Empires. The Treaty of Paris (1763) gave Great Britain rights to all land east of the Mississippi and Spain rights to land west of the Mississippi. Spain also ceded Florida to Britain to regain Cuba, which the British occupied during the war. Britain then divided the territory into East and West Florida.

Article 8 of the Treaty of Paris (1783) states, "The navigation of the river Mississippi, from its source to the ocean, shall forever remain free and open to the subjects of Great Britain and the citizens of the United States". With this treaty, which ended the American Revolutionary War, Britain also ceded West Florida back to Spain to regain The Bahamas, which Spain had occupied during the war. Spain then had control over the river, south of 32°30' north latitude and in what is known as the Spanish Conspiracy, hoped to gain greater control of Louisiana and all of the west. These hopes ended when Spain was pressured into signing Pinckney's Treaty in 1795.

19th century

France reacquired 'Louisiana' from Spain in the secret Treaty of San Ildefonso in 1800. The United States bought the territory from France in the Louisiana Purchase of 1803. In 1815, the U.S. defeated Britain at the Battle of New Orleans, part of the War of 1812, securing American control of the river.

So many settlers traveled westward through the Mississippi river basin, as well as settled in it, that Zadok Cramer wrote a guide book called The Navigator, detailing the features and dangers and navigable waterways of the area. It was so popular that he updated and expanded it through 12 editions over a period of 25 years.

Shifting sand bars made early navigation difficult.

Steamboat commerce

Mark Twain's book, Life on the Mississippi, covered the steamboat commerce which took place from 1830 to 1870 on the river before more modern ships replaced the steamer. The book was published first in serial form in Harper's Weekly in seven parts in 1875. The full version, including a passage from the unfinished Adventures of Huckleberry Finn and works from other authors, was published by James R. Osgood & Company in 1885.

The first steamboat to travel the full length of the Mississippi from the Ohio River to New Orleans was the New Orleans in December 1811. Its maiden voyage occurred during the series of New Madrid earthquakes in 1811–12.

Steamboat transport remained a viable industry, both in terms of passengers and freight until the end of the first decade of the 20th century. Among the several Mississippi River system steamboat companies was the noted Anchor Line, which from 1859 to 1898 operated a luxurious fleet of steamers between St. Louis and New Orleans.

Civil War

Battle of Vicksburg (ca. 1888)

The river played a decisive role in the American Civil War. The Union's Vicksburg Campaign called for Union control of the lower Mississippi River. The Union victory at the Battle of Vicksburg in Warren County, Mississippi in 1863 was pivotal to the Union's final victory of the Civil War.

20th century

In the spring of 1927, the river broke out of its banks in 145 places, during the Great Mississippi Flood of 1927 and inundated 27,000 sq mi (70,000 km2) to a depth of up to 30 ft (9.1 m).

On October 20, 1976, the automobile ferry, MV George Prince, was struck by a ship traveling upstream as the ferry attempted to cross from Destrehan, Louisiana, to Luling, Louisiana. Seventy-eight passengers and crew died, only eighteen survived the accident.

In 1988, record low water levels provided an opportunity and obligation to examine the climax of the wooden-hulled age. The Mississippi fell to 10 feet (3.0 m) below zero on the Memphis gauge. Four and a half acres of water craft remains were exposed on the bottom of the Mississippi River at West Memphis, Arkansas. They dated to the late 19th to early 20th centuries. The State of Arkansas, the Arkansas Archeological Survey, and the Arkansas Archeological Society responded with a two-month data recovery effort. The fieldwork received national media attention as good news in the middle of a drought.[18]

The Great Flood of 1993 was another significant flood, primarily affecting the Mississippi above its confluence with the Ohio River at Cairo, Illinois.

Two portions of the Mississippi were designated as American Heritage Rivers in 1997: the lower portion around Louisiana and Tennessee, and the upper portion around Iowa, Illinois, Minnesota and Missouri.

Campsite at the river in Arkansas

21st century

In 2002, Slovenian long-distance swimmer, Martin Strel, swam the entire length of the river, from Minnesota to Louisiana, over the course of 68 days.

In 2005, the Source to Sea Expedition [4] paddled the Mississippi and Atchafalaya Rivers to benefit the Audubon Society's Upper Mississippi River Campaign.[19][20]

On August 1, 2007, the I-35W Mississippi River bridge in Minneapolis collapsed during the evening rush hour.

Recreation

Water skiing

Great River Road in Wisconsin near Lake Pepin (2005)

The sport of water skiing was invented on the river in a wide region between Minnesota and Wisconsin known as Lake Pepin.[21] Ralph Samuelson of Lake City, Minnesota, created and refined his skiing technique in late June and early July 1922. He later performed the first water ski jump in 1925 and was pulled along at 80 mph (130 km/h) by a Curtiss flying boat later that year.[21]

National parks

There are seven National Park Service sites along the Mississippi River. The Mississippi National River and Recreation Area is the National Park Service site dedicated to protecting and interpreting the Mississippi River itself. The other six National Park Service sites along the river are (listed from north to south):

Navigation history

A clear channel is needed for the barges and other vessels that make the main stem Mississippi one of the great commercial waterways of the world. The task of maintaining a navigation channel is the responsibility of the United States Army Corps of Engineers, which was established in 1802.[22] Earlier projects began as early as 1829 to remove snags, close off secondary channels and excavate rocks and sandbars.

Steamboats entered trade in the 1820s, so the period 1830 – 1850 became the golden age of steamboats. As there were few roads or rails in the lands of the Louisiana Purchase, river traffic was an ideal solution. Cotton, timber and food came down the river, as did Appalachia coal. The port of New Orleans boomed as it was the trans-shipment point to deep sea ocean vessels. As a result, the image of the twin stacked, wedding cake Mississippi steamer entered into American mythology. Steamers worked the entire route from the trickles of Montana, to the Ohio river; down the Missouri and Tennessee. To the main channel of the Mississippi. Only the arrival of the railroads in the 1880s did steamboat traffic diminish. Steamboats remained a feature until the 1920s. Most have been superseded by pusher tugs. A few survive as icons—the Delta Queen and the River Queen for instance.

A series of 29 locks and dams on the upper Mississippi, most of which were built in the 1930s, is designed primarily to maintain a 9 feet (2.7 m) deep channel for commercial barge traffic.[23][24] 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.

Barges on the Mississippi River near Ste. Genevieve, Missouri.

19th century

Obstacles – Des Moines, Iowa/Illinois

In 1829, there were surveys of the two major obstacles on the upper Mississippi, the Des Moines Rapids and the Rock Island Rapids, where the river was shallow and the riverbed was rock. The Des Moines Rapids were about 11 mi (18 km) long and just above the mouth of the Des Moines River at Keokuk, Iowa. The Rock Island Rapids were between Rock Island and Moline, Illinois. Both rapids were considered virtually impassable.

In 1848, the Illinois and Michigan Canal was built to connect the Mississippi River to Lake Michigan via the Illinois River near Peru, Illinois. In 1900, the canal was replaced by the Chicago Sanitary and Ship Canal. The canal allowed Chicago to address specific health issues (typhoid fever, cholera and other waterborne diseases) by sending its waste down the Illinois and Mississippi river systems rather than polluting its water source of Lake Michigan. The canal also provided a shipping route between the Great Lakes and the Mississippi.

The Corps of Engineers recommended the excavation of a 5 ft (1.5 m) deep channel at the Des Moines Rapids, but work did not begin until after Lieutenant Robert E. Lee endorsed the project in 1837. The Corps later also began excavating the Rock Island Rapids. By 1866, it had become evident that excavation was impractical, and it was decided to build a canal around the Des Moines Rapids. The canal opened in 1877, but the Rock Island Rapids remained an obstacle.

In 1878, Congress authorized the Corps to establish a 4.5 feet (1.4 m) deep channel to be obtained by building wing dams which direct the river to a narrow channel causing it to cut a deeper channel, by closing secondary channels and by dredging. The channel project was complete when the Moline Lock, which bypassed the Rock Island Rapids, opened in 1907.

Canal – St. Paul, Minnesota

To improve navigation between St. Paul, Minnesota, and Prairie du Chien, Wisconsin, the Corps constructed several dams on lakes in the headwaters area, including Lake Winnibigoshish and Lake Pokegama. The dams, which were built beginning in the 1880s, stored spring run-off which was released during low water to help maintain channel depth.

In 1907, Congress authorized a 6 feet (1.8 m) deep channel project on the Mississippi, which was not complete when it was abandoned in the late 1920s in favor of the 9 feet (2.7 m) deep channel project.

20th century

Dam –Keokuk, Iowa

In 1913, construction was complete on a dam at Keokuk, Iowa, the first dam below St. Anthony Falls. Built by a private power company to generate electricity, the Keokuk dam was one of the largest hydro-electric plants in the world at the time. The dam also eliminated the Des Moines Rapids.

Lock and Dam Nos. 1 & 2

Lock and Dam No. 1 was completed in Minneapolis, Minnesota in 1917. Lock and Dam No. 2, near Hastings, Minnesota was completed in 1930.

1927 flood

Prior to the 1927 flood, the Corps' primary strategy was to close off as many side channels as possible to increase the flow in the main river. It was thought that the river's velocity would scour off bottom sediments, deepening the river and decreasing the possibility of flooding.

The 1927 flood proved this to be so wrong that communities threatened by the flood began to create their own levee breaks to relieve the force of the rising river.

Rivers and Harbors Act – 1930

The Rivers and Harbors Act of 1930 authorized the 9 feet (2.7 m) channel project, which called for a navigation channel 9 ft (2.7 m) deep and 400 ft (120 m) wide to accommodate multiple-barge tows.[25][26]

This was achieved by a series of locks and dams, and by dredging. Twenty-three new locks and dams were built on the upper Mississippi in the 1930s in addition to the three already in existence.

Late 20th century

A low-water dam deepens the pool above the Chain of Rocks Lock near St. Louis (2006)
Soldiers of the Missouri Army National Guard sandbag the River in Clarksville, Missouri, June 2008, following flooding.

Until the 1950s, there was no dam below Lock and Dam 26 at Alton, Illinois. Chain of Rocks Lock (Lock and Dam No. 27), which consists of a low-water dam and an 8.4 mi (13.5 km) long canal, was added in 1953, just below the confluence with the Missouri River, primarily to bypass a series of rock ledges at St. Louis. It also serves to protect the St. Louis city water intakes during times of low water.

U.S. government scientists determined in the 1950s that the Mississippi River was starting to switch to the Atchafalaya River channel because of its much steeper path to the Gulf of Mexico. Eventually the Atchafalaya River would capture the Mississippi River and become its main channel to the Gulf of Mexico, leaving New Orleans on a side channel. As a result, the U.S. Congress authorized a project called the Old River Control Structure, which has prevented the Mississippi River from leaving its current channel that drains into the Gulf via New Orleans.[27]

Because the large scale of high-energy water flow threatened to damage the structure, an auxiliary flow control station was built adjacent to the standing control station. This US$ 300 million project was completed in 1986 by the U.S. Army Corps Of Engineers.

Beginning in the 1970s, the Corps applied hydrological transport models to analyze flood flow and water quality of the Mississippi.

Dam 26 at Alton, Illinois, which had structural problems, was replaced by the Mel Price Lock and Dam in 1990. The original Lock and Dam 26 was demolished.

21st century

Main floodways

The Corps now actively creates floodways to divert periodic water surges into backwater channels and lakes. The main floodways are the Birds Point-New Madrid Floodway, the Morganza Spillway, which directs floodwaters down the Atchafalaya River and the Bonnet Carré Spillway which directs water to Lake Pontchartrain.

The Old River Control Structure also serve as a major floodgates that can be opened to prevent flooding. Some of the pre-1927 strategy is still in use today, the Corps actively cuts the necks of horseshoe bends, allowing the water to move faster and reducing flood heights.

In popular culture

Literature

  • William Faulkner uses the Mississippi River and Delta as the setting for many hunts throughout his novels. It has been proposed that in Faulkner's famous story, The Bear, young Ike first begins his transformation into a man, thus relinquishing his birthright to land in Yoknapatawpha County through his realizations found within the woods surrounding the Mississippi River.
  • Many of the works of Mark Twain deal with or take place near the Mississippi River. One of his first major works, Life on the Mississippi, is in part a history of the river, in part a memoir of Twain's experiences on the river, and a collection of tales that either take place on or are associated with the river. The river was noted for the number of bandits which called its islands and shores home, including John Murrell who was a well-known murderer, horse stealer and slave "re-trader". His notoriety was such that author Twain devoted an entire chapter to him in Life on the Mississippi, and Murrell was rumored to have an island headquarters on the river at Island 37. Twain's most famous work, Adventures of Huckleberry Finn, is largely a journey down the river. The novel works as an episodic meditation on American culture with the river having multiple different meanings including independence, escape, freedom, and adventure.
  • Herman Melville's novel The Confidence-Man portrayed a Canterbury Tales-style group of steamboat passengers whose interlocking stories are told as they travel down the Mississippi River. The novel is written both as cultural satire and a metaphysical treatise. Like Huckleberry Finn, it uses the Mississippi River as a metaphor for the larger aspects of American and human identity that unify the otherwise disparate characters. The river's fluidity is reflected by the often shifting personalities and identities of Melville's "confidence man".

Music

On The Mississippi, music sheet cover for a 1912 song
  • The stage and movie musical Show Boat's central musical piece is the spiritual-influenced ballad "Ol' Man River".
  • The musical Big River is based on the travels of Huckelberry Finn down the river.
  • Ferde Grofé composed a set of movements for symphony orchestra based on the lands the river travels through in his "Mississippi Suite".
  • The Johnny Cash song "Big River" is about the Mississippi River, and about drifting the length of the river to pursue a relationship that fails.
  • "Mississippi Queen" by the rock group Mountain makes reference to the river.
  • The song "When the Levee Breaks", made famous in the version performed by Led Zeppelin on the album Led Zeppelin IV, was composed by Memphis Minnie McCoy in 1929 after the Great Mississippi Flood of 1927. Another song about the flood was "Louisiana 1927" by Randy Newman for the album Good Old Boys.
  • "Roll On Mississippi" and "Mississippi Cotton Picking Delta Town" are two classics from Charlie Pride that refer to the Mississippi River.
  • In one of his books, DuBose Heyward claims that jazz got its name from a black itinerant musician called Jazbo Brown. Around the turn of the 19th century the semi-legendary Brown is said to have played on boats along the Mississippi River, as suggested in "Jazzbo Brown from Memphis Town", performed by Bessie Smith.

See also

References

Notes

  1. ^ The United States Geological Survey recognizes two contrasting definitions of a river's source.[1] By the stricter definition, the Mississippi would share its source with its longest tributary, the Missouri, at Brower's Spring in Montana. The other definition acknowledges "somewhat arbitrary decisions" and places the Mississippi's source at Lake Itasca, which is publicly accepted as the source,[2] and which had been identified as such by Brower himself.[3]
  2. ^ Median of the 1,826 daily mean streamflows recorded by the USGS for the period 1978–1983 at Baton Rouge.
  3. ^ United States Geological Survey Hydrological Unit Code: 08-09-01-00- Lower Mississippi-New Orleans Watershed
  4. ^ a b "Lengths of the major rivers". United States Geological Survey. http://ga.water.usgs.gov/edu/riversofworld.html. Retrieved 2009-03-14. 
  5. ^ U.S. Army Corps of Engineers navigation charts. 2300 miles from Lake Itasca to Head of Passes -- Southwest Pass is 20 miles.
  6. ^ http://encyclopediaofarkansas.net/encyclopedia/entry-detail.aspx?entryID=2546 encyclopediaofarkansas.net
  7. ^ http://www.yale.edu "Treaty of Friendship, Limits, and Navigation" , Avalon project at the Yale Law School
  8. ^ Mississippi River Facts
  9. ^ 2001 US Army Corps of Engineers Upper Mississippi River Navigation Chart
  10. ^ Costello, Mary Charlotte (2002). Climbing the Mississippi River Bridge by Bridge, Volume Two: Minnesota. Cambridge, MN: Adventure Publications. ISBN 0-9644518-2-4. 
  11. ^ "General Information about the Mississippi River". Mississippi National River and Recreation Area. National Park Service. 2004. http://www.nps.gov/miss/features/factoids/. Retrieved 2006-07-15. 
  12. ^ Americas Wetland: Resource Center
  13. ^ "Freelang Ojibwe Dictionary". http://www.freelang.net/dictionary/ojibwe.html. 
  14. ^ "Mississippi". American Heritage Dictionary. Yourdictionary.com. http://www.yourdictionary.com/ahd/m/m0343500.html. Retrieved 2007-03-06. 
  15. ^ Gilfillan, Joseph A. "Minnesota Geographical Names Derived from the Chippewa Language" in The Geological and Natural History Survey of Minnesota: The Fifteenth Annual Report for the Year 1886 (St. Paul: Pioneer Press Company, 1887)
  16. ^ http://www.cec.org/naatlas/NA-Watersheds.gif Cec.org
  17. ^ "Pierre Le Moyne, Sieur d'Iberville" (bio), webpage from The Catholic Encyclopedia, Volume VII, 1910, New York: CathEn-07614b.
  18. ^ UA-WRI Research Station, Historical Archeology. "Ghost Boats of the Mississippi". http://www.uark.edu/campus-resources/archinfo/atughostboats.html. 
  19. ^ "Upper Mississippi River Campaign". National Audubon Society. 2006. http://www.audubon.org/campaign/umr. Retrieved 2006-11-29. 
  20. ^ "Paddling the Mississippi River to Benefit the Audubon Society". Source to Sea: The Mississippi River Project. Source to Sea 2006. 2006. http://www.sourcetosea.net. Retrieved 2006-11-29. 
  21. ^ a b "The Beginning". USA Water Ski.org. 2009. http://www.usawaterski.org/pages/USA-WS%20Profile.htm. Retrieved 30 July 2009. 
  22. ^ http://www.hq.usace.army.mil/history/brief.html
  23. ^ "Mississippi River". USGS: Status and trends of the nation's biological resources. http://biology.usgs.gov/s+t/SNT/noframe/ms137.htm. Retrieved 2007-02-03. 
  24. ^ "U.S. Waterway System Facts, December 2005" (PDF). USACE Navigation Data Center. http://www.iwr.usace.army.mil/ndc/factcard/fc05/factcard.pdf. Retrieved 2006-04-27. 
  25. ^ "The Mississippi and its Uses". Natural Resource Management Section, Rock Island Engineers. http://www.mvr.usace.army.mil/missriver/Interp/MissUses.htm. Retrieved 2006-06-21. 
  26. ^ "Appendix E: Nine-foot navigation channel maintenance activities". National Park Service, Mississippi National River and Recreation Area Comprehensive Management Plan. http://www.nps.gov/miss/info/cmp/appendices/appendix_e.html. Retrieved 2006-06-21. 
  27. ^ "The Old River Control Structure on the Lower Mississippi River". www.sjsu.edu. http://www.sjsu.edu/faculty/watkins/oldriver.htm. Retrieved 2009-06-12. 

Bibliography

  • Anfinson, John O.; Thomas Madigan, Drew M. Forsberg, and Patrick Nunnally (2003). The River of History: A Historic Resources Study of the Mississippi National River and Recreation Area. St. Paul, MN: U.S. Army Corps of Engineers, St. Paul District. OCLC 53911450. 
  • Bartlett, Richard A. (1984). Rolling rivers: an encyclopedia of America's rivers. New York: McGraw-Hill. ISBN 0-07-003910-0. OCLC 10807295. 
  • Penn, James R. (2001). Rivers of the world: a social, geographical, and environmental sourcebook. Santa Barbara, Calif.: ABC-CLIO. ISBN 1-57607-042-5. OCLC 260075679. 
  • Smith, Thomas Ruys (2007). River of dreams: imagining the Mississippi before Mark Twain. Baton Rouge: Louisiana State University Press. ISBN 978-0-8071-3233-3. OCLC 182615621. 

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