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The Illinois River

A Comprehensive Study of a Vital Waterway: Exploring its hydrography, geology, rich history, and its crucial role in commerce, transportation, and ecology.

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Overview

A Principal Tributary

The Illinois River is a principal tributary of the Mississippi River, stretching approximately 273 miles (439 km) across the U.S. state of Illinois.5 Its extensive drainage basin covers 28,756.6 square miles (72,700 km2), encompassing parts of Illinois, Wisconsin, Indiana, and Michigan.6 The river originates from the confluence of the Des Plaines and Kankakee Rivers within the Chicago metropolitan area and flows southwestward, ultimately joining the Mississippi River near Grafton, Illinois.23

Lifeline of Commerce

Historically and presently, the Illinois River has served as a critical transportation corridor. It forms the backbone of the Illinois Waterway, linking the Great Lakes to the Mississippi River system. This connection facilitates the movement of bulk goods such as grain and oil, supporting significant commercial shipping operations. Major river ports, including Peoria, are situated along its banks.13

Ecological Significance

The river's banks host important natural areas, such as Starved Rock State Park and the Emiquon Complex, recognized for their ecological value. Historically, the river was a rich source of aquatic life, supporting extensive fishing and mussel harvesting industries. While facing challenges from pollution and invasive species like Asian carp, it remains an important waterway for recreation and sports fishing.16

Hydrography

Course and Confluence

The Illinois River is formed by the confluence of the Kankakee River and the Des Plaines River in Grundy County, Illinois.7 Its journey takes it westward through cities like Morris and Ottawa, where it receives the Mazon and Fox Rivers, respectively. Further west, the Vermilion River joins the flow near LaSalle. After a significant turn south in Bureau County, known as the "Great Bend," the river meanders southwestward past major cities like Peoria, Pekin, and Havana, before eventually merging with the Mississippi River near Grafton.23

Dimensions and Flow

The river's physical characteristics are substantial:

Key Hydrological Data
Length 273 mi (439 km)
Basin Size 28,756.6 sq mi (72,700 km2)
Source Elevation 505 ft (154 m)
Mouth Elevation 417 ft (127 m)
Average Discharge (Valley City) 23,280 cu ft/s (659 m3/s)1
Maximum Discharge Recorded 123,000 cu ft/s (3,500 m3/s)1
Minimum Discharge Recorded 1,330 cu ft/s (38 m3/s)1

1 Data from USGS Gage #05586100 at Valley City, IL (1939-2012).1

Major Tributaries

The Illinois River is fed by numerous tributaries that contribute to its significant flow and drainage basin. Key tributaries include:

  • Left Bank: Kankakee River, Mazon River, Vermilion River, Mackinaw River, Sangamon River.
  • Right Bank: Des Plaines River, Fox River, Illinois and Michigan Canal (historically significant).

Its mouth is at the Mississippi River near Grafton, Illinois.27

Geology

Ancient River Channels

The current path of the Illinois River south of Hennepin largely follows the ancient channel of the Mississippi River. During the Illinoian Stage (approximately 300,000 to 132,000 years ago), glacial activity diverted the Mississippi from its original course near Rock Island, forcing it into its present-day channel. Following the glacier's retreat, the Illinois River occupied this former Mississippi channel.8

The Kankakee Torrent

The dramatic formation of the modern Illinois River channel is attributed to the Kankakee Torrent, a massive glacial lake outburst flood that occurred around 18,500 years ago during the melting of the Wisconsin Glacier.8 A large proglacial lake, comparable in size to one of the modern Great Lakes, formed behind a terminal moraine in present-day Indiana. As glacial meltwater increased, the lake overflowed the moraine, leading to a catastrophic dam burst that carved the river's deep canyon in a matter of days.9 This event created a channel far larger than necessary for the river's current flow, leaving behind striking rock formations.

History

Indigenous and Colonial Routes

The Illinois River valley has been a vital transportation artery for millennia. Indigenous peoples utilized portages between the Des Plaines and Chicago Rivers, and the Kankakee and St. Joseph Rivers, to connect the Great Lakes with the Mississippi basin.10 The first European presence was marked by Father Jacques Marquette's Jesuit mission in 1675 near Starved Rock. French explorers like Renรฉ-Robert Cavelier, Sieur de La Salle, established forts, such as Fort St. Louis, to facilitate the fur trade and defend the region.11 The Illinois Confederation were the primary inhabitants of this fertile valley, which Marquette described as abundant in resources and wildlife.10

Canals and Industrial Growth

Before the completion of the Illinois and Michigan Canal in 1845, Peoria was the sole major settlement on the river, with trade primarily flowing downstream to St. Louis. The canal's construction significantly shifted Chicago's influence westward, fostering the growth of cities like LaSalle, Peru, and Ottawa along the river.12 During the 19th and early 20th centuries, river towns thrived on harvesting fish, waterfowl, mussels (for the button industry), and ice. This dependence fostered industries like tourism, commercial fishing, and early refrigeration.12

Waterway Modernization

The late 19th century saw the construction of the Chicago Sanitary and Ship Canal, which reversed the flow of the Chicago River, directing the city's sewage into the Illinois River.12 While the original Illinois and Michigan Canal eventually declined, it was replaced by the Illinois Waterway in 1933, a system of locks and dams that continues to support navigation and commercial shipping today. This waterway is managed by the U.S. Army Corps of Engineers and is a vital component of the Great Loop, enabling circumnavigation of Eastern North America.13

Modern Use

Commercial Navigation

The Illinois Waterway, utilizing the Illinois River, remains a crucial artery for commercial transport. Barges laden with bulk commodities like grain and petroleum products traverse the system daily. The eight locks and dams operated by the U.S. Army Corps of Engineers manage river traffic and flood control, ensuring the waterway's functionality.13

Recreation and Ecology

The river is a popular destination for recreational boating, particularly for those navigating the Great Loop. It also supports a significant sports fishing industry, known for its sauger fishery. However, ecological challenges persist. Overfishing, heavy siltation, and water pollution have impacted native species. Invasive Asian carp pose a significant threat, crowding out game fish.16 Efforts are ongoing to manage combined sewer overflows from cities like Peoria to improve water quality, adhering to Clean Water Act requirements.1718

Interpretation and Education

Institutions like the Peoria Riverfront Museum, with its "Illinois River Encounter" gallery, and the Starved Rock Lock and Dam Visitor Center offer exhibits detailing the river's geology, ecology, history, and engineering. These centers provide valuable insights into the river's complex ecosystem and its role in regional development.1415

Cities and Towns

Communities Along the Waterway

Numerous communities have developed along the banks of the Illinois River, each contributing to its rich tapestry of history and commerce. Key cities and towns include:

  • Bath
  • Beardstown
  • Browning
  • Chillicothe
  • Chicago
  • Channahon
  • Creve Coeur
  • East Peoria
  • Florence
  • Grafton
  • Hardin
  • Havana
  • Hennepin
  • Henry
  • Kampsville
  • Kingston Mines
  • LaSalle
  • Lacon
  • Liverpool
  • Marseilles
  • Meredosia
  • Morris
  • Naplate
  • Naples
  • North Utica
  • Oglesby
  • Ottawa
  • Pearl
  • Pekin
  • Peoria
  • Peoria Heights
  • Peru
  • Rome
  • Seneca
  • Spring Bay
  • Spring Valley
  • Valley City

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References

References

A full list of references for this article are available at the Illinois River Wikipedia page

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Disclaimer

Important Notice

This page has been generated by an Artificial Intelligence and is intended for informational and educational purposes only. The content is derived from publicly available data, primarily the Wikipedia article on the Illinois River, and may not be entirely accurate, complete, or up-to-date. While efforts have been made to refine and polish the information, it is based on a snapshot of data and should not be considered definitive.

This is not professional advice. The information provided on this website is not a substitute for professional hydrological, geological, historical, environmental, or engineering consultation. Always refer to official documentation, consult with qualified experts, and conduct independent research for specific project needs or academic requirements. Never disregard professional advice or delay in seeking it because of information found on this website.

The creators of this page are not responsible for any errors or omissions, or for any actions taken based on the information provided herein. Users are encouraged to verify information from primary sources.