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{{Geobox|River
{{Geobox|River
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|name = Mississippi River
|name = Cole Peterson
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|country = United States
|country = United States
|country_flag = 1
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|state = Minnesota
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|discharge_location = [[Baton Rouge, Louisiana|Baton Rouge, LA]]
|discharge_location = [[Baton Rouge, Louisiana|Baton Rouge, LA]]
|discharge_imperial = 651000
|discharge_imperial = 651000
|discharge_max_imperial = 3195000
|discharge_max_imperial =A lot of water
|discharge_min_imperial = 159000
|discharge_min_imperial = 159000
|discharge_note =<ref name="USGSrivers">{{cite web
|discharge_note =<ref name="USGSrivers">{{cite web

Revision as of 14:54, 22 March 2011

For the river in Canada, see Mississippi River (Ontario).

Template:Geobox

The Mississippi River is the largest river system in North America.[1][2] About 2,320 miles (3,730 km) long,[3] the river originates at Lake Itasca, Minnesota, and flows slowly southwards in sweeping meanders, terminating 95 miles (153 km) by river below New Orleans, 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–US 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 Laurentide 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 many different names, it was the Ojibwe word misi-ziibi, meaning Great River, or gichi-ziibi, meaning Big River, that ultimately gave the river its present-day name. European explorers reached the mouth of the river as early as the 16th century and 17th century. 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 20th 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 in preventing 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 in Minneapolis. 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 upper Mississippi is a cascade of reservoirs, as are many of its tributaries like the Missouri and Tennessee.

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.

Geography

The confluence of the Mississippi and Ohio rivers at Cairo, Illinois is the demarcation between the upper and the lower Mississippi River.

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 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.[4][5] 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.[6] 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.[2] 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. At the confluence, the Ohio is even bigger than the Mississippi itself (long term mean discharge of the Ohio at Cairo: 281,500 cu ft/s (7,970 m3/s) [7]; long term mean discharge of the Mississippi at Thebes: 208,200 cu ft/s (5,900 m3/s) [8]) and, thus, is hydrologically the main stream of the whole river system, also including the Allegheny River further upstream.

The Mississippi River is divided into the upper Mississippi and the lower Mississippi.

Upper Mississippi River

Main article: Upper Mississippi River
The beginning of the Mississippi River at Lake Itasca (2004)

The Mississippi River from its source to the confluence of the Ohio River at the southern tip of the state of Illinois is called The Upper Mississippi River.[9] It is divided into three sections:

  1. The headwaters, 493 miles (793 km), from the source to Saint Anthony Falls
  2. A series of man-made lakes between Minneapolis, Minnesota and St. Louis, Missouri, 664 miles (1,069 km)
  3. The middle Mississippi, 190 miles (310 km), a relatively free-flowing river from the confluence with the Missouri River at St. Louis, Missouri to the confluence of the Ohio River.

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).[10] The lake is fed by a number of smaller streams, sometimes considered the river's source.

Coon Rapids Dam
Mississippi Head of Navigation: Coon Rapids Dam

The head of navigation on the Mississippi is the Coon Rapids Dam in Coon Rapids, Minnesota. Before its construction in 1913 steamboats could occasionally go upstream as far as Saint Cloud, depending on river conditions.

They 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.[11] 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

See also: Mississippi River Delta

The Mississippi River from the confluence of the Ohio River to its mouth at the Gulf of Mexico is called the Lower Mississippi River.

Tributaries

The major tributaries of the Lower Mississippi River are the White River, flowing in at the White River National Wildlife Refuge in east central Arkansas; the Arkansas River, joining the Mississippi at Arkansas Post; the Yazoo River, meeting the Mississippi at Vicksburg, Mississippi, and the Red River;.

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

See also: List of crossings of the Upper Mississippi River and List of crossings of the Lower Mississippi River
File:Minn04.jpg
The Stone Arch Bridge, the Third Avenue Bridge and the Hennepin Avenue Bridge in Minneapolis (2004)
The Dubuque-Wisconsin Bridge connecting Dubuque, Iowa and Grant County, Wisconsin (2004)
Norbert F. Beckey bridge at Muscatine with LED lighting
The Hernando de Soto Bridge in Memphis, Tennessee (2009)
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.[12]

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.

John James Audubon Bridge – Pointe Coupee Parish, Louisiana and West Feliciana Parish, Louisiana is under construction, when finished it will be the longest bridge on the Mississippi River.

Watershed

Mississippi watershed (2005)
See also: List of drainage basins by area

The Mississippi River has the fourth 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. The total catchment of the Mississippi River covers nearly 40% of the landmass of the continental United States.

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.[13]

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).[14] 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 40 times the volume of the Colorado River.

Sediment

Prior to 1900, the Mississippi River transported an estimated 400 million metric tons of sediment per year from the interior of the United States to coastal Louisiana and the Gulf of Mexico. During the last two decades, this number was only 145 million metric tons per year. The reduction in sediment transported down the Mississippi River is the result of engineering modification of the Mississippi, Missouri, and Ohio rivers and their tributaries by dams, meander cutoffs, river-training structures, and bank revetments and soil erosion control programs in the areas drained by them.[15]

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

Ojibwe Wigwam at Grand Portage– oil on canvas by Eastman Johnson (1857)

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 Máʼxe-éʼometaaʼe (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).[16][17]

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.[18] 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

Ca. 1681 map of Marquette and Jolliet's 1673 expedition.

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.[19]

French explorers, Louis Jolliet and Jacques Marquette, began exploring the Mississippi in the 17th century. Marquette traveled with a Sioux who named it 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.[20] 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. In 1800, under duress from Napoleon of France, Spain ceded an undefined portion of West Florida to France. When France then sold the Louisiana Territory to the US in 1803, a dispute arose again between Spain and the US on which parts of West Florida exactly had Spain ceded to France, which would in turn decide which parts of West Florida were now US property versus Spanish property. These aspirations 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.

Breaching the continental divide

When Louis Jolliet explored the Mississippi Valley in the 17th century, natives guided him to a quicker way to return to French Canada via the Illinois River. When he found the Chicago Portage, he remarked that a canal of "only half a league" (less than 2 miles (3.2 km), 3 km) would join the Mississippi and the Great Lakes.[21] In 1848, the continental divide separating the waters of the Great Lakes and the Mississippi Valley was breached by the Illinois and Michigan canal via the Chicago River.[22] This both accelerated the development, and forever changed the ecology of the Mississippi Valley and the Great Lakes.

Steamboat commerce

Main article: Steamboats of the Mississippi

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)

Control of the river was a strategic objective of both sides in the American Civil War. In 1862 Union's forces coming down the river successfully cleared Confederate defenses at Island Number 10 and Memphis, Tennessee, while Naval forces coming upriver from the Gulf of Mexico captured New Orleans, Louisiana. The remaining major Confederate stronghold was on the heights overlooking the river at Vicksburg, Mississippi, and the Union's Vicksburg Campaign (December 1862 to July, 1863) completed control of the lower Mississippi River. The Union victory ending the Siege of Vicksburg on July 4, 1863 was pivotal to the Union's final victory of the Civil War.

20th century

The "Big Freeze" of 1918/19 blocked river traffic north of Memphis, Tennessee, preventing transportation of coal from southern Illinois. This resulted in widespread shortages, high prices, and rationing of coal in January and February.[23]

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. Water craft remains were exposed in an area of 4.5 acres (18,000 m2) 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.[24]

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 [1] paddled the Mississippi and Atchafalaya Rivers to benefit the Audubon Society's Upper Mississippi River Campaign.[25][26]

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.[27] 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.[27]

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.[28] 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 Appalachian 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.[29][30] 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

Lock and Dam No. 11, north of Dubuque, Iowa (2007)

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 at Keokuk, Iowa

Main article: Lock and Dam No. 19

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. 2, near Hastings, Minnesota (2007)

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

Main article: Great Mississippi Flood of 1927

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.[31][32]

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

File:A03 4696 683x1024.JPG
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.[33]

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.

Usage 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

File:On-The-Mississippi-.jpg
On The Mississippi, music sheet cover for a 1912 song
  • 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.
  • Ferde Grofé composed a set of movements for symphony orchestra based on the lands the river travels through in his "Mississippi Suite".
  • 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 Huckleberry Finn down the river.
  • 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.
  • "Roll On Mississippi" and "Mississippi Cotton Picking Delta Town" are two classics from Charley 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.
  • The late Conway Twitty and Loretta Lynn collaborated on the song "Louisiana Woman, Mississippi Man" about lovers separated by the mighty river, but are not afraid to swim it, even at the risk of alligator bites, at a one-mile (1.6 km) wide juncture separating the two states, for a rendezvous.

See also

References

Notes
  1. ^ United States Geological Survey Hydrological Unit Code: 08-09-01-00- Lower Mississippi-New Orleans Watershed
  2. ^ a b "Lengths of the major rivers". United States Geological Survey. Retrieved 2009-03-14.
  3. ^ U.S. Army Corps of Engineers navigation charts. 2,300 miles (3,700 km) from Lake Itasca to Head of Passes – Southwest Pass is 20 miles (32 km).
  4. ^ "encyclopediaofarkansas.net". encyclopediaofarkansas.net. 2010-04-28. Retrieved 2010-11-06.
  5. ^ Yale.edu "Treaty of Friendship, Limits, and Navigation" , Avalon project at the Yale Law School
  6. ^ "Mississippi River Facts". Nps.gov. Retrieved 2010-11-06.
  7. ^ Frits van der Leeden, Fred L. Troise, David Keith Todd: The Water Encyclopedia, 2nd edition, p 126, Chelsea, Mich. (Lewis Publishers), 1990, ISBN 0-87371-120-3
  8. ^ USGS stream gage 07022000 Mississippi River at Thebes, IL[dead link]
  9. ^ "Mississippi River".
  10. ^ Upham, Warren. "Minnesota Place Names: A Geographical Encyclopedia". Minnesota Historical Society. Retrieved 2007-08-14.
  11. ^ 2001 US Army Corps of Engineers Upper Mississippi River Navigation Chart
  12. ^ Costello, Mary Charlotte (2002). Climbing the Mississippi River Bridge by Bridge, Volume Two: Minnesota. Cambridge, MN: Adventure Publications. ISBN 0-9644518-2-4.
  13. ^ "General Information about the Mississippi River". Mississippi National River and Recreation Area. National Park Service. 2004. Retrieved 2006-07-15.
  14. ^ "Americas Wetland: Resource Center". Americaswetlandresources.com. 1939-11-04. Retrieved 2010-11-06.
  15. ^ Meade, R. H., and J. A. Moody, 1984, Causes for the decline of suspended-sediment discharge in the Mississippi River system, 1940–2007 Hydrology Processes vol. 24, pp. 35–49.
  16. ^ "Freelang Ojibwe Dictionary".
  17. ^ "Mississippi". American Heritage Dictionary. Yourdictionary.com. Archived from the original on 2007-02-20. Retrieved 2007-03-06.
  18. ^ 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)
  19. ^ Cec.org[dead link]
  20. ^ "Pierre Le Moyne, Sieur d'Iberville" (bio), webpage from The Catholic Encyclopedia, Volume VII, 1910, New York: CathEn-07614b.
  21. ^ "Jolliet and La Salle's Canal Plans". Encyclopedia.chicagohistory.org. Retrieved 2010-11-06.
  22. ^ "Illinois & Michigan Canal National Heritage Corridor". Nps.gov. 1984-08-24. Retrieved 2010-11-06.
  23. ^ "Southeast Missouri State University: The Big Freeze, 1918–1919". Semo.edu. Retrieved 2010-11-06.
  24. ^ UA-WRI Research Station, Historical Archeology. "Ghost Boats of the Mississippi".
  25. ^ "Upper Mississippi River Campaign". National Audubon Society. 2006. Archived from the original on November 24, 2006. Retrieved 2006-11-29.
  26. ^ "Paddling the Mississippi River to Benefit the Audubon Society". Source to Sea: The Mississippi River Project. Source to Sea 2006. 2006. Retrieved 2006-11-29.
  27. ^ a b "The Beginning". USA Water Ski.org. 2009. Retrieved 30 July 2009.
  28. ^ "US Army Corps of Engineers, Brief History". Usace.army.mil. Retrieved 2010-11-06.
  29. ^ "Mississippi River". USGS: Status and trends of the nation's biological resources. Archived from the original on September 27, 2006. Retrieved 2007-02-03.
  30. ^ "U.S. Waterway System Facts, December 2005" (PDF). USACE Navigation Data Center. Retrieved 2006-04-27.
  31. ^ "The Mississippi and its Uses". Natural Resource Management Section, Rock Island Engineers. Retrieved 2006-06-21.
  32. ^ "Appendix E: Nine-foot navigation channel maintenance activities". National Park Service, Mississippi National River and Recreation Area Comprehensive Management Plan. Retrieved 2006-06-21.
  33. ^ "The Old River Control Structure on the Lower Mississippi River". www.sjsu.edu. Retrieved 2009-06-12.
Bibliography
  • Anfinson, John O. (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. {{cite book}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  • 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.

Scott, Quinta (2010). The Mississippi: A Visual Biography. Columbia, Missouri: University of Missouri Press. ISBN 978-0-8262-1840-7. OCLC 277196207.

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