Illinois Basin

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American Paleozoic depositional and structural basin

title: "Illinois Basin" type: doc version: 1 created: 2026-02-28 author: "Wikipedia contributors" status: active scope: public tags: ["coal-mining-regions-in-the-united-states", "geologic-formations-of-illinois", "geologic-formations-of-indiana", "geologic-formations-of-kentucky", "geologic-provinces-of-the-united-states", "mining-in-illinois", "oil-fields-of-the-united-states", "paleozoic-illinois", "paleozoic-indiana", "paleozoic-kentucky", "paleozoic-united-states", "sedimentary-basins-of-north-america", "structural-basins-of-the-united-states"] description: "American Paleozoic depositional and structural basin" topic_path: "philosophy" source: "https://en.wikipedia.org/wiki/Illinois_Basin" license: "CC BY-SA 4.0" wikipedia_page_id: 0 wikipedia_revision_id: 0

::summary American Paleozoic depositional and structural basin ::

::data[format=table title="Infobox sedimentary basin"]

FieldValue
nameIllinois Basin
named_forIllinois
imageIllinois Basin Structure Map.jpg
image_captionBasin structure map
pushpin_mapUnited States#Illinois
pushpin_relief1
map_imageIllinoisBasinMap.jpg
map_captionLocation of the Illinois Basin (USGS)
column_imageIllinois Basin Pennsylvanian stratigraphy.jpg
column_captionPennsylvanian stratigraphy
section_imageIllinois Basin Pennsylvanian strata cross section.jpg
section_captionIllinois Basin cross-section
coordinates
country
stateIllinois, SW Indiana, W Kentucky
onoffshoreOnshore
boundariesKankakee Arch (NE), Cincinnati Arch (SE)
Pascola Arch (S), Ozark Dome (SW)
Mississippi River Arch (NW), Wisconsin Arch (N)
area80000 sqmi
plateNorth American Plate
ageCambrian-Pennsylvanian
stratigraphyStratigraphy
fieldsCoal fields
faultsNew Madrid seismic zone, Wabash Valley seismic zone
::

| name = Illinois Basin | other_name = | named_for = Illinois | image = Illinois Basin Structure Map.jpg | image_size = | image_alt = | image_caption = Basin structure map | pushpin_map = United States#Illinois | pushpin_map_size = | pushpin_map_alt = | pushpin_map_caption = | pushpin_relief = 1 | pushpin_mark = | pushpin_mark_size = | pushpin_label = | pushpin_label_position = | map_image = IllinoisBasinMap.jpg | map_size = | map_alt = | map_caption = Location of the Illinois Basin (USGS) | column_image = Illinois Basin Pennsylvanian stratigraphy.jpg | column_size = | column_alt = | column_caption = Pennsylvanian stratigraphy | section_image = Illinois Basin Pennsylvanian strata cross section.jpg | section_size = | section_alt = | section_caption = Illinois Basin cross-section | coordinates = | location = | region = | country = | state = Illinois, SW Indiana, W Kentucky | cities = | onoffshore = Onshore | boundaries = Kankakee Arch (NE), Cincinnati Arch (SE) Pascola Arch (S), Ozark Dome (SW) Mississippi River Arch (NW), Wisconsin Arch (N) | partof = | seas = | rivers = | lakes = | area = 80000 sqmi | basin_type = | plate = North American Plate | orogeny = | age = Cambrian-Pennsylvanian | stratigraphy = Stratigraphy | fields = Coal fields | faults = New Madrid seismic zone, Wabash Valley seismic zone | footnotes = | embed =

The Illinois Basin is a Paleozoic depositional and structural basin in the United States, centered in and underlying most of the state of Illinois, and extending into southwestern Indiana and western Kentucky. The basin is elongate, extending approximately 400 mi northwest-southeast, and 200 mi southwest-northeast.

Boundaries and sedimentary rocks

::figure[src="https://upload.wikimedia.org/wikipedia/commons/1/11/New_Albany_Stratigraphy.png" caption="Devonian [[stratigraphic column"] ::

The basin is bordered on the northeast by the Kankakee Arch, on the southeast by the Cincinnati Arch, on the south by the Pascola Arch, on the southwest by the Ozark Dome, on the northwest by the Mississippi River Arch, and on the north by the Wisconsin Arch. The New Madrid seismic zone and the Wabash Valley seismic zone intersect the southern portion of the basin.

The major structural features within the basin include the La Salle anticlinal belt, the DuQuoin monocline, the Cottage Grove fault system, and the Fairfield Basin.

At its center beneath southern Illinois, the basin contains a thickness of about 15,000 feet of Cambrian through Pennsylvanian sedimentary rocks, predominantly marine, and mostly dolomite, limestone, shale, and sandstone.

The basement rocks deep below the sedimentary rocks of the basin are Proterozoic granites and rhyolite of the Eastern Granite–Rhyolite Province which dates to around 1.55 Ga.

Mineral resources

The rocks of the Illinois Basin are sources of coal, petroleum, and other minerals.

Coal

Bituminous coal is present in Pennsylvanian rocks in the basin, deposited in freshwater swamp environments. Over the years, the Illinois Basin has produced more than eight billion tons of coal in Southern Illinois, particularly in the Harrisburg Coal Field, and the Western Coal Fields of Kentucky. Coal production was 99 million short tons in 2008, roughly equally divided between Illinois, Indiana, and western Kentucky. The basin provided 8% of US coal production in 2008.

Petroleum

::figure[src="https://upload.wikimedia.org/wikipedia/commons/c/c1/Emma_Township_pumpjacks.jpg" caption="Pumpjacks operating in [[White County, Illinois"] ::

The Illinois Basin has produced more than four billion barrels of petroleum. Waterflooding of old reservoirs caused a third peak of oil production in the 1950s.

Much recent drilling activity has targeted shale gas in the Devonian-Mississippian New Albany Shale.

Non-fuel minerals

The rocks of the Illinois Basin are thought to be the source of metals in Mississippi Valley-Type lead-zinc deposits, both within the basin and in surrounding areas, such as the Lead Belt of southeast Missouri.

Within the basin, deposits valuable for lead, zinc, coal balls and fluorite are mined in Hardin and Pope counties, Illinois, and Crittenden and Livingston counties, Kentucky. the deposits are in the form of veins and limestone replacement deposits in Mississippian sedimentary rocks. Ore minerals are fluorite, galena, and sphalerite. Gangue minerals include common quartz and calcite, and minor barite and chalcopyrite.

Carbon sequestration

Some geologic formations in the Illinois Basin are considered to have potential for carbon sequestration, as a permanent disposal site for carbon dioxide that would otherwise be released into the atmosphere. In 2009, Archer Daniels Midland Corp. began pilot testing the carbon sequestration potential of the Mt. Simon formation beneath its ethanol manufacturing facility in Illinois. As of January 2015, one million metric tons of carbon dioxide had been sequestered in the Illinois Basin-Decatur Project.

References

References

  1. (1987). "Thrust faults in southern Illinois basin -- result of contemporary stress?". USGS.
  2. (2002). "Geologic Overview, Chapter C of Resource Assessment of the Springfield, Herrin, Danville, and Baker Coals in the Illinois Basin, U.S. Geological Survey Professional Paper 1625–D". USGS.
  3. David H. Swann, "A summary geologic history of the Illinois Basin," in ''Geology and Petroleum Production of the Illinois Basin'', Illinois Geologic Society, 1968, p.3-21.
  4. Van Schmus, W.R., et al., 2007, ''New insights into the southern margin of the Archean–Proterozoic boundary in the north-central United States based on U-Pb, Sm-Nd, and Ar-Ar geochronology'', Precambrian Research, v. 157, p. 80–105, {{doi. 10.1016/j.precamres.2007.02.011.
  5. Ben A. Van der Pluijm, Paul A. Catacosinos, ''Basement and basins of eastern North America'', Geological Society of America, Special Paper 308, 1996, p. 14 {{ISBN. 978-0-8137-2308-2
  6. US Geological Survey, [https://energy.usgs.gov/factsheets/Illinois/illinois.basin.html ''A rebirth of the Illinois Basin''], retrieved 29 October 2009.
  7. F. Freme, "Coal review," ''Mining Engineering'', May 2009, p.52.
  8. Major oil production began in 1905, and from 1907 through 1912, the basin was the third-most oil productive area in the United States. Oil production peaked in 1908 at 34 million barrels per year, and declined steadily to 5 million barrels in 1933. A new wave of exploration brought oil production to a new high of 140 million barrels in 1940, after which production again declined.[[Harold F. Williamson]] and others, ''The American Petroleum Industry, 1899-1958'', Evanstion, Ill.: Northwestern Univ. Press, 1963, p.16, 25, 540.
  9. Robert M. Grogan and James C. Bradbury, "Fluorite-zinc-lead deposits of the Illinois-Kentucky mining district," in ''Ore Deposits in the United States'', New York: American Institute of Mining, Metallurgical, and Petroleum Engineers (AIME), 1968, v.1, p.370-399.
  10. Archer Daniels Midland, [http://www.adm.com/en-US/responsibility/enviro_stewardship/Pages/Carbon.aspx Carbon-sequestration projects put innovative emissions-reduction technology to the test] {{Webarchive. link. (2010-01-03 , accessed 26 February 2010)
  11. "One million metric tons of CO2 stored underground in Illinois - KurzweilAI". kurzweilai.net.

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coal-mining-regions-in-the-united-statesgeologic-formations-of-illinoisgeologic-formations-of-indianageologic-formations-of-kentuckygeologic-provinces-of-the-united-statesmining-in-illinoisoil-fields-of-the-united-statespaleozoic-illinoispaleozoic-indianapaleozoic-kentuckypaleozoic-united-statessedimentary-basins-of-north-americastructural-basins-of-the-united-states