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Geology of Illinois : ウィキペディア英語版
Geology of Illinois

The strata of the bedrock geology of Illinois are dominated by Pennsylvanian age rocks which occur within the Illinois Basin.
== Illinois Basin ==
The Illinois Basin is a northwest-southeast asymmetrical structural basin that is filled with more than 4000 meters of Paleozoic sedimentary rocks. The basin covers most of Illinois, and extends into western Indiana and western Kentucky. The basin is bounded to the north by the Mississippi River and the Kankakee Arch, to the east by the Cincinnati Arch, and to the south by the Ozark uplift and Pascola Arch.〔(McDowell, R.C., (ed.), 2001, The geology of Kentucky -- A text to accompany the geologic map of Kentucky: USGS Professional Paper 1151-H, 68 p. )〕

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