Inside Illinois: Mineral ResourcesIllinois State Geological Survey
Science
Inside Illinois: Mineral Resources
Illinois State Geological Survey
Mines and mineral resources -- Illinois
The structure and nature of coke make it a valuable fuel for blast
furnace use in the production of steel. In the past, most of the coal
used in the manufacture of coke has come from areas of higher quality
coal outside of our state. However, at present, over 1,000,000 tons of
Illinois coal are mined annually for the production of metallurgical
coke.
[Illustration: Figure 12—Estimated total coal production by counties
from 1882 through 1963.]
Area underlain by coal-bearing rocks
Counties producing coal in January 1965
Total Production 3,749,423,534 tons
71 counties producing
STONE AND STONE PRODUCTS
WHAT TYPES OF STONE ARE PRODUCED IN ILLINOIS?
Limestone and dolomite are the most abundant rocks quarried in Illinois.
Small amounts of marble, limestone, and sandstone for building stone are
also produced. In addition, some glacial boulders and cobbles are used
for rock gardens and in home construction. The crushed limestone
industry is Illinois’ most important rock products industry.
WHAT ARE LIMESTONE AND DOLOMITE?
Limestone is a sedimentary rock that consists chiefly of calcite, which
is composed of calcium, carbon, and oxygen. Dolomite is a variety of
limestone that contains considerable magnesium in addition to the other
elements. Limestones were deposited on the floors of ancient seas that
repeatedly covered most parts of Illinois. Shelled creatures, corals,
and coral reefs helped build up the thick limestone deposits (figs. 13
and 14).
[Illustration: Figure 13—Piece of limestone largely made up of
fossil brachiopod shells.]
WHERE ARE LIMESTONE AND DOLOMITE QUARRIES LOCATED IN ILLINOIS?
Limestone and dolomite quarries are located along the southern, western,
and northern margins of the state where the thick deposits of these
rocks crop out at the surface. Although bedrock was deposited in
horizontal layers, it has since been downfolded into the Illinois Basin
whose center is in southeastern Illinois. Thus, the thick limestones and
dolomites that are quarried along the margins of the state are too
deeply buried to be quarried in the central part of this basin (fig.
15).
[Illustration: Figure 14—Fossils commonly found in Illinois rocks.]
_Strophomena_ 1×
_Paleoneilo_ 1×
_Ctenodonta_ ⅔×
_Dolmanites_ ½×
_Archimedes_ 1×
_Hormotoma Polygyra_ 1×
_Mucrospirifer_ 1½×
_Atrypa_ ⅔×
_Crinoid Columnais_ 1×
_Halysites_ ⅔×
_Hexagonaria_ 1×
_Microcylus_ 1×
_Streptelasma_ ⅔×
_Lithostrationella_ ½×
_Lophophyllum_ 1×
[Illustration: Figure 15—Diagrammatic cross section of the Illinois
Basin.]
_MISS. RIVER_
Waterloo
Mt. Vernon
ILLINOIS
_WABASH RIVER_
INDIANA
New Albany
_OHIO RIVER_
ARE ANY STONE QUARRIES LOCATED IN THE AREA UNDERLAIN BY THE ILLINOIS
BASIN?
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