McCormick Group: Difference between revisions

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{{DISPLAYTITLE:McCormick Group (abandoned)}}
{{Tree
{{Tree
|category1=Paleozoic Erathem
|category1=Abandoned Names
|category2=Pennsylvanian Subsystem
|category3=Absaroka Sequence
|category4=McCormick Group
|tree1=McCormick Group
|tree1=McCormick Group
|tree21=Paleozoic Erathem
|tree21=Paleozoic Erathem
|tree22=Pennsylvanian Subsystem
|tree22=Pennsylvanian Subsystem
|tree23=Morrowan Series
|tree31=Absaroka Sequence
|tree31=Absaroka Sequence
}}
}}
==Primary source==
==Primary source==
Willman, H. B., Elwood Atherton, T. C. Buschbach, Charles Collinson, John C. Frye, M. E. Hopkins, Jerry A. Lineback, and Jack A. Simon, 1975, Handbook of Illinois Stratigraphy: Illinois State Geological Survey Bulletin 95, 261 p.
Nelson, W.J., P.H. Heckel and J.M. Obrad, 2022, Pennsylvanian Subsystem in Illinois: Illinois State Geological Survey, Bulletin (in press).


==Contributing author(s)==
==Contributing author(s)==
M. E. Hopkins and J. A. Simon
W.J. Nelson


==Name==
==Name==


===Original description===
===Original description===
The McCormick Group (Kosanke et al., 1960, p. 28).
Kosanke et al. (1960, p. 28) established the McCormick Group, comprised of the Caseyville Formation and the newly designated [[Abbott Formation]] overlying the Caseyville. Compared with the overlying [[Kewanee Group]] (also newly named, but now also abandoned), the McCormick contained a greater proportion of sandstone, thinner and more lenticular shale and limestone, and less marked cyclicity.


===Derivation===
===Derivation===
Named for McCormick in northwestern Pope County, where the various units of this group are prominently exposed.
The name alludes to the settlement of McCormick in northwestern Pope County, southern Illinois. Christian L. McCormic (no “k”) settled here in the 1880s and established a general store. A gristmill, hoop mill, blacksmith shop, and post office followed. McCormick boomed in the 1920s, when the Illinois Central Railroad built the Edgewood Cutoff and hundreds of workers drove a tunnel and deep cuts through the Shawnee Hills. After the railroad was completed, people moved away and the businesses closed (Sneed 1977). Today, McCormick is a small cluster of houses.


===Other names===
===Other names===
None. This name was never used outside Illinois.


===History/background===
===History/background===
With abandonment of the [[Abbott Formation]] (Nelson et al. 1991; Tri-State Committee 2001), the McCormick Group lost its upper portion. A group cannot contain only part of a formation (in this case, the Tradewater). Thus, having standardized the upper boundary, the Tri-State Committee extended the [[Raccoon Creek Group]] throughout the Illinois Basin and abandoned use of the McCormick Group.


==Type section==
==Type section==
 
Kosanke et al. (1960, p. 44) listed “Vicinity of McCormick, NW part of [Pope] County” but did not describe the section. Reference can be made to type sections of the Caseyville (Lee 1916) and [[Abbott Formation|Abbott]] (Kosanke et al. 1960). Appropriately, the latter consists of exposures along the Edgewood Cutoff past the site of McCormick.
===Type location===
 
===Type author(s)===
 
===Type status===
 
==Reference section==
 
===Reference location===
 
===Reference author(s)===
 
===Reference status===
 
==Stratigraphic relationships==
In Illinois the McCormick Group comprises strata of the Caseyville and Abbott Formations, from the base of the Pennsylvanian to the top of the Bernadotte Sandstone Member (fig. P-2). The McCormick Group comprises strata formerly included in the Tradewater and Caseyville Groups (Wanless, 1939; Weller, 1940).
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{| class="wikitable" style="text-align: center;"
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|<gallery caption="" widths=250px heights=250px perrow=4>
Figure P-2.jpg|{{file:Figure P-2.jpg}}
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==Extent and thickness==
The McCormick Group in Illinois thickens from about 200 feet at the northwestern extent of the Pennsylvanian to at least 600 feet in southern Illinois, but it is absent in substantial areas in both western and northern Illinois.
 
==Lithology==
Lithologically, this group is almost entirely detrital. It is made up of 50-60 percent massive, predominantly cross-bedded, relatively pure quartz sandstone and 40 percent or more sandy shale and siltstone. The sandstones are seldom more than 100 feet thick. A few thin, nonpersistent coals and rare fossiliferous limestones occur locally. Several of the fine-grained sandstones and a few shales are calcareous in places and contain marine invertebrate fossils, but the bulk of the units of the McCormick Group are barren of animal fossils.
 
==Core&#40;s&#41;==
 
==Photograph&#40;s&#41;==
 
==Contacts==
 
==Well log characteristics==
 
==Fossils==
 
==Age and correlation==
 
==Environments of deposition==
 
==Economic importance==
 
==Remarks==


==References==
==References==
KOSANKE, R. M., J. A. SIMON, H. R. WANLESS, and H. B. WILLMAN, 1960, Classification of the Pennsylvanian strata of Illinois: Illinois State Geological Survey Report of Investigations 214, 84 p.<br>
* Kosanke, R.M., J.A. Simon, H.R. Wanless, and H.B. Willman, 1960, Classification of the Pennsylvanian strata of Illinois: Illinois State Geological Survey, Report of Investigations 214, 84 p., 1 pl.<br>
WANLESS, H. R., 1939, Pennsylvanian correlations in the Eastern Interior and Appalachian coal fields: Geological Society of America Special Paper 17, 130 p.<br>
* Lee, W., 1916, Geology of the Shawneetown Quadrangle in Kentucky: Kentucky Geological Survey, Ser. 4, v. 4, part 2, 73 p.<br>
WELLER, J. M., 1940, Geology and oil possibilities of extreme southern Illinois: Illinois State Geological Survey Report of Investigations 71, 71 p.
* Nelson, W.J., J.A. Devera, R.J. Jacobson, D.K. Lumm, R.A. Peppers, B. Trask, C.P. Weibel, L.R. Follmer, M.H. Riggs, S.P. Esling, E.D. Henderson, and M.S. Lannon, 1991, Geology of the Eddyville, Stonefort, and Creal Springs Quadrangles, southern Illinois: Illinois State Geological Survey, Bulletin 96, 85 p., 1 pl.<br>
* Sneed, G.J., 1977, Ghost towns of southern Illinois: Royalton, Illinois, G.J. Sneed, 309 p.<br>
* Tri-State Committee, 2001, Toward a more uniform stratigraphic nomenclature for rock units (formations and groups) of the Pennsylvanian System in the Illinois Basin: Illinois, Indiana, and Kentucky Geological Surveys, Illinois Basin Consortium Study 5, 26 p.<br>


{{Codes
{{Codes

Latest revision as of 16:14, 9 February 2022

Lithostratigraphy: McCormick Group
Chronostratigraphy: Paleozoic Erathem >>Pennsylvanian Subsystem >>Morrowan Series
Allostratigraphy: Absaroka Sequence

Primary source

Nelson, W.J., P.H. Heckel and J.M. Obrad, 2022, Pennsylvanian Subsystem in Illinois: Illinois State Geological Survey, Bulletin (in press).

Contributing author(s)

W.J. Nelson

Name

Original description

Kosanke et al. (1960, p. 28) established the McCormick Group, comprised of the Caseyville Formation and the newly designated Abbott Formation overlying the Caseyville. Compared with the overlying Kewanee Group (also newly named, but now also abandoned), the McCormick contained a greater proportion of sandstone, thinner and more lenticular shale and limestone, and less marked cyclicity.

Derivation

The name alludes to the settlement of McCormick in northwestern Pope County, southern Illinois. Christian L. McCormic (no “k”) settled here in the 1880s and established a general store. A gristmill, hoop mill, blacksmith shop, and post office followed. McCormick boomed in the 1920s, when the Illinois Central Railroad built the Edgewood Cutoff and hundreds of workers drove a tunnel and deep cuts through the Shawnee Hills. After the railroad was completed, people moved away and the businesses closed (Sneed 1977). Today, McCormick is a small cluster of houses.

Other names

None. This name was never used outside Illinois.

History/background

With abandonment of the Abbott Formation (Nelson et al. 1991; Tri-State Committee 2001), the McCormick Group lost its upper portion. A group cannot contain only part of a formation (in this case, the Tradewater). Thus, having standardized the upper boundary, the Tri-State Committee extended the Raccoon Creek Group throughout the Illinois Basin and abandoned use of the McCormick Group.

Type section

Kosanke et al. (1960, p. 44) listed “Vicinity of McCormick, NW part of [Pope] County” but did not describe the section. Reference can be made to type sections of the Caseyville (Lee 1916) and Abbott (Kosanke et al. 1960). Appropriately, the latter consists of exposures along the Edgewood Cutoff past the site of McCormick.

References

  • Kosanke, R.M., J.A. Simon, H.R. Wanless, and H.B. Willman, 1960, Classification of the Pennsylvanian strata of Illinois: Illinois State Geological Survey, Report of Investigations 214, 84 p., 1 pl.
  • Lee, W., 1916, Geology of the Shawneetown Quadrangle in Kentucky: Kentucky Geological Survey, Ser. 4, v. 4, part 2, 73 p.
  • Nelson, W.J., J.A. Devera, R.J. Jacobson, D.K. Lumm, R.A. Peppers, B. Trask, C.P. Weibel, L.R. Follmer, M.H. Riggs, S.P. Esling, E.D. Henderson, and M.S. Lannon, 1991, Geology of the Eddyville, Stonefort, and Creal Springs Quadrangles, southern Illinois: Illinois State Geological Survey, Bulletin 96, 85 p., 1 pl.
  • Sneed, G.J., 1977, Ghost towns of southern Illinois: Royalton, Illinois, G.J. Sneed, 309 p.
  • Tri-State Committee, 2001, Toward a more uniform stratigraphic nomenclature for rock units (formations and groups) of the Pennsylvanian System in the Illinois Basin: Illinois, Indiana, and Kentucky Geological Surveys, Illinois Basin Consortium Study 5, 26 p.

ISGS Codes

Stratigraphic Code Geo Unit Designation
3530
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