Potsdam Sandstone Megagroup

From ILSTRAT
Revision as of 20:54, 11 January 2017 by Jennifer.Obrad (talk | contribs) (→‎Name)

(diff) ← Older revision | Approved revision (diff) | Latest revision (diff) | Newer revision → (diff)
Jump to navigation Jump to search

Lithostratigraphy: Potsdam Sandstone Megagroup
Chronostratigraphy: Paleozoic Erathem >>Cambrian System >>Croixan Series >>Dresbachian Stage
Allostratigraphy: Sauk 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)

T. C. Buschbach

Name

Original description

Potsdam Sandstone Megagroup (Emmons, 1838, p. 214-217, 230).

Derivation

Named for Potsdam, St. Lawrence County, New York.

Other names

History/background

The name "Potsdam" was widely used in early reports for the basal Cambrian sandstone, but later its use was restricted to the type region. It was reinstated for the megagroup by Swann and Willman (1961) (figs. 14 and Є-3).

Type section

Type location

Type author(s)

Type status

Reference section

Reference location

Reference author(s)

Reference status

Stratigraphic relationships

The Potsdam Sandstone Megagroup consists of the dominantly sandstone formations that compose the lower part of the Cambrian strata in the Illinois Basin. Traced southward from southern Wisconsin, where the entire Cambrian section is included in the Potsdam, the clastics become finer grained and grade to dolomite that is included in the Knox Megagroup. Throughout most of Illinois, however, the megagroups are separated by a zone of mixed dolomite, siltstone, and sandstone that is not included in either group. In the northern tier of counties in Illinois, the top of the Potsdam is commonly the top of the Franconia Formation. In the rest of the northern and in the central part of the state, the top is placed at the top of the lowest member (Elmhurst) of the Eau Claire Formation. In southern Illinois, the top of the Potsdam is the top of the Mt. Simon Sandstone.

Extent and thickness

The Potsdam Sandstone Megagroup underlies all of Illinois but is not exposed. It has a maximum thickness of more than 2600 feet in northeastern Illinois.

Lithology

Core(s)

Photograph(s)

Contacts

Well log characteristics

Fossils

Age and correlation

Environments of deposition

Economic importance

Remarks

References

EMMONS, EBENEZER, 1838, Report of the Second Geological District of the State of New York: New York Geological Survey, 2nd Annual Report, p. 186-252.
SWANN, D. H., and H. B. WILLMAN, 1961, Megagroups in Illinois: American Association of Petroleum Geologists Bulletin, v. 45, p. 471-483; Illinois State Geological Survey Reprint 1961-N.

ISGS Codes

Stratigraphic Code Geo Unit Designation
8650
--