Wilhelmi Formation

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Lithostratigraphy: Hunton Limestone Megagroup >>Wilhelmi Formation
Chronostratigraphy: Paleozoic Erathem >>Silurian System >>Alexandrian Series
Allostratigraphy: Tippecanoe Sequence

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.

Contributing author(s)

H. B. Willman and Elwood Atherton

Name

Original description

Derivation

The Wilhelmi Formation is named for Wilhelmi Airport on the south side of Joliet, Will County.

Other names

Earlier the Wilhelmi Formation had been referred to as the lower shaly part of the Edgewood Formation.

History/background

Type section

Type location

The type section of the Wilhelmi Formation is a railroad cut about 5 miles southwest of Wilhelmi Airport (SE SW SE 35, 35N-9E).

Type author(s)

Type status

Reference section

Reference location

Reference author(s)

Reference status

Stratigraphic relationships

Extent and thickness

The Wilhelmi Formation is as much as 100 feet thick where it fills deep channels in the Maquoketa Shale Group, but it is thin or absent in other areas. It is absent in southern Illinois.

Stratigraphic Position

The Wilhelmi Formation (Willman, 1973, p. 12) is the basal formation in the Alexandrian Series in northeastern Illinois (fig. S-3).

Lithology

The lower part of the Wilhelmi Formation is medium to dark gray, very argillaceous dolomite and dolomitic shale. This unit is differentiated as the Schweizer Member and is present only where the formation is thick. The overlying moderately argillaceous dolomite, differentiated as the Birds Member, is characteristic of the relatively thin part of the formation. In some areas the basal dolomitic shale is difficult to differentiate from shale of the underlying Maquoketa Group, but the latter generally is greenish gray.

Core(s)

Photograph(s)

Contacts

Well log characteristics

Fossils

The Wilhelmi contains early Llandoverian graptolites (Ross, 1962a).

Age and correlation

The Wilhelmi is lithologically similar to the Mosalem Formation in northwestern Illinois. It probably correlates with the lower part of the Edgewood Formation in western Illinois but is more argillaceous than the latter. Strata of similar lithology occur in the basal Edgewood in Iowa and are locally present in the base of the Mayville in Wisconsin and the Brassfield in Indiana and Kentucky.

Environments of deposition

Economic importance

Remarks

References

ROSS, C. A., 1962a, Early Llandoverian (Silurian) graptolites from the Edgewood Formation, northeastern Illinois: Journal of Paleontology, v. 36, no. 6, p. 1383-1386; Illinois State Geological Survey Reprint 1963-A.
WILLMAN, H. B., 1973, Rock stratigraphy of the Silurian System in northeastern and northwestern Illinois: Illinois State Geological Survey Circular 479, 55 p.

ISGS Codes

Stratigraphic Code Geo Unit Designation
6975
On