Tuscaloosa Formation

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Lithostratigraphy: Embayment Megagroup >>Tuscaloosa Formation
Chronostratigraphy: Mesozoic Erathem >>Cretaceous System >>Gulfian Series

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 John C. Frye

Name

Original description

The Tuscaloosa Formation (Smith and Johnson, 1887, p. 18, 95-117).

Derivation

Named for exposures along the Tuscaloosa (Black Warrior) River near Tuscaloosa, Alabama.

Other names

History/background

Type section

Type location

Type author(s)

Type status

Reference section

Reference location

Reference author(s)

Reference status

Stratigraphic relationships

Extent and thickness

It is exposed only locally in extreme southern Illinois and appears to have a patchy distribution (Pryor, 1960; Pryor and Ross, 1962; Ross, 1964). It has maximum thickness of 20 feet but is generally much thinner. The Tuscaloosa is well exposed along the Post Creek Cutoff, Pulaski County (cen. 2, 15S-2E), and in railroad cuts in the Thebes Gorge, 1 mile south of Rock Springs Hollow, Alexander County (SW 21, 15S-3W).

Lithology

It is largely chert gravel, generally moderately cemented with fine silica or white clay. The chert pebbles, in a matrix of coarse quartz sand, are mainly white or gray, but black pebbles are locally common. Beds of pebbly sand and white clay also are common. The clays are dominantly kaolinite (Pryor and Glass, 1961). The Little Bear Soil occurs in deposits at the base of the Tuscaloosa Formation. Gravel found northeast of Elco in northern Alexander County (SW SE 7, 14S-1W) is probably Tuscaloosa Gravel preserved in sink holes. Local concentrations of gray and black chert pebbles on the upland bedrock surfaces as far north as Kaolin, Union County (SW NW 2, 12S-2W), are probably residual or reworked from the Tuscaloosa.

Core(s)

Photograph(s)

Contacts

Well log characteristics

Fossils

Age and correlation

The Tuscaloosa in Illinois is similar in lithology and stratigraphic position to the Tuscaloosa of Kentucky and Tennessee, but it is a transgressive deposit and may be younger than the type Tuscaloosa.

Environments of deposition

Economic importance

Remarks

References

PRYOR, W. A., 1960, Cretaceous sedimentation in upper Mississippi Embayment: American Association of Petroleum Geologists Bulletin, v. 44, p. 1473-1504; Illinois State Geological Survey Reprint 1960-J.
PRYOR, W. A., and H. D. GLASS, 1961, Cretaceous-Tertiary clay mineralogy of the upper Mississippi Embayment: Journal of Sedimentary Petrology, v. 31, p. 36-51; Illinois State Geological Survey Reprint 1961-M.
PRYOR, W. A., and C. A. ROSS, 1962, Geology of the Illinois parts of the Cairo, La Center, and Thebes Quadrangles: Illinois State Geological Survey Circular 332, 39 p.
ROSS, C. A., 1964, Geology of the Paducah and Smithland Quadrangles in Illinois: Illinois State Geological Survey Circular 360, 32 p.
SMITH, E. A., and L. C. JOHNSON, 1887, Tertiary and Cretaceous strata of the Tuscaloosa, Tombigbee, and Alabama Rivers: USGS Bulletin 43, 189 p.

ISGS Codes

Stratigraphic Code Geo Unit Designation
1440
Kp