The Mitchell Plain is a
karst area in
Indiana
Indiana () is a U.S. state in the Midwestern United States. It is the 38th-largest by area and the 17th-most populous of the 50 States. Its capital and largest city is Indianapolis. Indiana was admitted to the United States as the 19th ...
of relatively low relief. The extensive underlying cave system developed in
Mississippian
Mississippian may refer to:
* Mississippian (geology), a subperiod of the Carboniferous period in the geologic timescale, roughly 360 to 325 million years ago
*Mississippian culture, a culture of Native American mound-builders from 900 to 1500 AD ...
age
limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms wh ...
bedrock. Surface drainage is rare due to most streams in the area disappearing into caves or joints within the rock.
The limestone is a vestige of an early shallow
craton
A craton (, , or ; from grc-gre, κράτος "strength") is an old and stable part of the continental lithosphere, which consists of Earth's two topmost layers, the crust and the uppermost mantle. Having often survived cycles of merging and ...
ic sea that covered what would become Indiana, while the North-South linearity of the region is left over from the
Cincinnati Uplift, sloping the rock layers from a high in the East sloping downward towards
Cairo, Illinois
Cairo ( ) is the southernmost city in Illinois and the county seat of Alexander County.
The city is located at the confluence of the Ohio and Mississippi rivers. Fort Defiance, a Civil War camp, was built here in 1862 by Union General Ulysse ...
.
The Mitchell Plain is bound by the older rocks of
Norman Upland on the East and the younger rocks of
Crawford Upland on the West.
References
Karst fields
Landforms of Indiana
Limestone formations of the United States
Geologic formations of Indiana
Mississippian United States
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