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Illinois Basin, the Glossary

Index Illinois Basin

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.[1]

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Table of Contents

  1. 58 relations: Anticline, Archer Daniels Midland, Baryte, Basement (geology), Bituminous coal, Calcite, Cambrian, Carbon dioxide, Carbon sequestration, Carbonate-hosted lead-zinc ore deposits, Chalcopyrite, Cincinnati Arch, Coal, Coal ball, Crittenden County, Kentucky, Devonian, Dolomite (rock), Fault (geology), Fluorite, Galena, Granite, Hardin County, Illinois, Harold F. Williamson, Harrisburg, Illinois, Illinois, Illinois Basin, Indiana, Kankakee Arch, Kentucky, Lead, Limestone, Livingston County, Kentucky, Mississippian (geology), Missouri, Monocline, New Albany Shale, New Madrid Seismic Zone, North American Plate, Ozarks, Paleozoic, Pennsylvanian (geology), Petroleum, Pope County, Illinois, Proterozoic, Quartz, Rhyolite, Sandstone, Sedimentary basin, Sedimentary rock, Shale, ... Expand index (8 more) »

  2. Coal mining regions in the United States
  3. Geologic formations of Illinois
  4. Geologic formations of Indiana
  5. Geologic formations of Kentucky
  6. Geologic provinces of the United States
  7. Mining in Illinois
  8. Oil fields of the United States
  9. Paleozoic Illinois
  10. Paleozoic Indiana
  11. Paleozoic Kentucky
  12. Paleozoic United States
  13. Sedimentary basins of North America
  14. Structural basins of the United States

Anticline

In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline.

See Illinois Basin and Anticline

Archer Daniels Midland

The Archer-Daniels-Midland Company, commonly known as ADM, is an American multinational food processing and commodities trading corporation founded in 1902 and headquartered in Chicago, Illinois.

See Illinois Basin and Archer Daniels Midland

Baryte

Baryte, barite or barytes is a mineral consisting of barium sulfate (BaSO4).

See Illinois Basin and Baryte

Basement (geology)

In geology, basement and crystalline basement are crystalline rocks lying above the mantle and beneath all other rocks and sediments.

See Illinois Basin and Basement (geology)

Bituminous coal

Bituminous coal, or black coal, is a type of coal containing a tar-like substance called bitumen or asphalt.

See Illinois Basin and Bituminous coal

Calcite

Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate (CaCO3).

See Illinois Basin and Calcite

Cambrian

The Cambrian is the first geological period of the Paleozoic Era, and the Phanerozoic Eon.

See Illinois Basin and Cambrian

Carbon dioxide

Carbon dioxide is a chemical compound with the chemical formula.

See Illinois Basin and Carbon dioxide

Carbon sequestration

Carbon sequestration is the process of storing carbon in a carbon pool.

See Illinois Basin and Carbon sequestration

Carbonate-hosted lead-zinc ore deposits

Carbonate-hosted lead-zinc ore deposits are important and highly valuable concentrations of lead and zinc sulfide ores hosted within carbonate (limestone, marl, dolomite) formations and which share a common genetic origin.

See Illinois Basin and Carbonate-hosted lead-zinc ore deposits

Chalcopyrite

Chalcopyrite is a copper iron sulfide mineral and the most abundant copper ore mineral.

See Illinois Basin and Chalcopyrite

Cincinnati Arch

The Cincinnati Arch is a broad structural uplift between the Illinois Basin to the west, the Michigan Basin to the northwest, and the Appalachian Basin and Black Warrior Basin to the east and southeast. Illinois Basin and Cincinnati Arch are geologic provinces of the United States.

See Illinois Basin and Cincinnati Arch

Coal

Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams.

See Illinois Basin and Coal

Coal ball

A coal ball is a type of concretion, varying in shape from an imperfect sphere to a flat-lying, irregular slab.

See Illinois Basin and Coal ball

Crittenden County, Kentucky

Crittenden County is a county in the U.S. state of Kentucky.

See Illinois Basin and Crittenden County, Kentucky

Devonian

The Devonian is a geologic period and system of the Paleozoic era during the Phanerozoic eon, spanning 60.3 million years from the end of the preceding Silurian period at million years ago (Ma), to the beginning of the succeeding Carboniferous period at Ma.

See Illinois Basin and Devonian

Dolomite (rock)

Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2.

See Illinois Basin and Dolomite (rock)

Fault (geology)

In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements.

See Illinois Basin and Fault (geology)

Fluorite

Fluorite (also called fluorspar) is the mineral form of calcium fluoride, CaF2.

See Illinois Basin and Fluorite

Galena

Galena, also called lead glance, is the natural mineral form of lead(II) sulfide (PbS).

See Illinois Basin and Galena

Granite

Granite is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase.

See Illinois Basin and Granite

Hardin County, Illinois

Hardin County is a county located in the U.S. state of Illinois.

See Illinois Basin and Hardin County, Illinois

Harold F. Williamson

Harold Francis Williamson Sr. (March 21, 1901 – October 25, 1989) was an American business historian, and Professor of American and European economic history at Northwestern University, most known for his 1963 work on the history of the American petroleum industry.

See Illinois Basin and Harold F. Williamson

Harrisburg, Illinois

Harrisburg is a city in and the county seat of Saline County, Illinois, United States.

See Illinois Basin and Harrisburg, Illinois

Illinois

Illinois is a state in the Midwestern region of the United States.

See Illinois Basin and Illinois

Illinois Basin

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. Illinois Basin and Illinois Basin are 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 and structural basins of the United States.

See Illinois Basin and Illinois Basin

Indiana

Indiana is a state in the Midwestern region of the United States.

See Illinois Basin and Indiana

Kankakee Arch

The Kankakee Arch is a geologic arch with a northwest–southeast trending axis which connects the Cincinnati Arch to the southeast with the Wisconsin Dome to the northwest.

See Illinois Basin and Kankakee Arch

Kentucky

Kentucky, officially the Commonwealth of Kentucky, is a landlocked state in the Southeastern region of the United States.

See Illinois Basin and Kentucky

Lead

Lead is a chemical element; it has symbol Pb (from Latin plumbum) and atomic number 82.

See Illinois Basin and Lead

Limestone

Limestone (calcium carbonate) is a type of carbonate sedimentary rock which is the main source of the material lime.

See Illinois Basin and Limestone

Livingston County, Kentucky

Livingston County is a county located in the U.S. state of Kentucky.

See Illinois Basin and Livingston County, Kentucky

Mississippian (geology)

The Mississippian (also known as Lower Carboniferous or Early Carboniferous) is a subperiod in the geologic timescale or a subsystem of the geologic record.

See Illinois Basin and Mississippian (geology)

Missouri

Missouri is a landlocked state in the Midwestern region of the United States.

See Illinois Basin and Missouri

Monocline

A monocline (or, rarely, a monoform) is a step-like fold in rock strata consisting of a zone of steeper dip within an otherwise horizontal or gently dipping sequence.

See Illinois Basin and Monocline

New Albany Shale

The New Albany Shale is an organic-rich geologic formation of Devonian and Mississippian age in the Illinois Basin of the United States.

See Illinois Basin and New Albany Shale

New Madrid Seismic Zone

The New Madrid Seismic Zone (NMSZ), sometimes called the New Madrid Fault Line, is a major seismic zone and a prolific source of intraplate earthquakes (earthquakes within a tectonic plate) in the Southern and Midwestern United States, stretching to the southwest from New Madrid, Missouri.

See Illinois Basin and New Madrid Seismic Zone

North American Plate

The North American Plate is a tectonic plate containing most of North America, Cuba, the Bahamas, extreme northeastern Asia, and parts of Iceland and the Azores.

See Illinois Basin and North American Plate

Ozarks

The Ozarks, also known as the Ozark Mountains, Ozark Highlands or Ozark Plateau, is a physiographic region in the U.S. states of Missouri, Arkansas, Oklahoma and the extreme southeastern corner of Kansas.

See Illinois Basin and Ozarks

Paleozoic

The Paleozoic (or Palaeozoic) Era is the first of three geological eras of the Phanerozoic Eon.

See Illinois Basin and Paleozoic

Pennsylvanian (geology)

The Pennsylvanian (also known as Upper Carboniferous or Late Carboniferous) is, on the ICS geologic timescale, the younger of two subperiods of the Carboniferous Period (or the upper of two subsystems of the Carboniferous System).

See Illinois Basin and Pennsylvanian (geology)

Petroleum

Petroleum or crude oil, also referred to as simply oil, is a naturally occurring yellowish-black liquid mixture of mainly hydrocarbons, and is found in geological formations.

See Illinois Basin and Petroleum

Pope County, Illinois

Pope County is the southeasternmost county in the U.S. state of Illinois.

See Illinois Basin and Pope County, Illinois

Proterozoic

The Proterozoic is the third of the four geologic eons of Earth's history, spanning the time interval from 2500 to 538.8Mya, the longest eon of the Earth's geologic time scale.

See Illinois Basin and Proterozoic

Quartz

Quartz is a hard, crystalline mineral composed of silica (silicon dioxide).

See Illinois Basin and Quartz

Rhyolite

Rhyolite is the most silica-rich of volcanic rocks.

See Illinois Basin and Rhyolite

Sandstone

Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains, cemented together by another mineral.

See Illinois Basin and Sandstone

Sedimentary basin

Sedimentary basins are region-scale depressions of the Earth's crust where subsidence has occurred and a thick sequence of sediments have accumulated to form a large three-dimensional body of sedimentary rock.

See Illinois Basin and Sedimentary basin

Sedimentary rock

Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation.

See Illinois Basin and Sedimentary rock

Shale

Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2Si2O5(OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.

See Illinois Basin and Shale

Shale gas

Shale gas is an unconventional natural gas that is found trapped within shale formations.

See Illinois Basin and Shale gas

Southeast Missouri Lead District

The Southeast Missouri Lead District, commonly called the Lead Belt, is a lead mining district in the southeastern part of Missouri.

See Illinois Basin and Southeast Missouri Lead District

Southern Illinois

Southern Illinois is a region of the U.S. state of Illinois comprising the southern third of the state, principally south of Interstate 70.

See Illinois Basin and Southern Illinois

Sphalerite

Sphalerite is a sulfide mineral with the chemical formula.

See Illinois Basin and Sphalerite

Structural basin

A structural basin is a large-scale structural formation of rock strata formed by tectonic warping (folding) of previously flat-lying strata into a syncline fold.

See Illinois Basin and Structural basin

Wabash Valley Seismic Zone

The Wabash Valley Seismic Zone (also known as the Wabash Valley Fault System or Zone) is a tectonic region located in the Midwestern United States, centered on the valley of the Lower Wabash River, along the state line between southeastern Illinois and southwestern Indiana.

See Illinois Basin and Wabash Valley Seismic Zone

Western Coal Field

The West Kentucky Coal Field comprises an area in the west-central and northwestern part of the state, bounded by the Dripping Springs Escarpment and the Pennyroyal Plateau and the Ohio River, but is part of the Illinois Basin that extends into Indiana and Illinois. Illinois Basin and Western Coal Field are coal mining regions in the United States.

See Illinois Basin and Western Coal Field

Zinc

Zinc is a chemical element with the symbol Zn and atomic number 30.

See Illinois Basin and Zinc

See also

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

References

[1] https://en.wikipedia.org/wiki/Illinois_Basin

Also known as Fairfield Basin, The Illinois Basin.

, Shale gas, Southeast Missouri Lead District, Southern Illinois, Sphalerite, Structural basin, Wabash Valley Seismic Zone, Western Coal Field, Zinc.