Ogle Till Member

(Redirected from 0910)
Jump to navigation Jump to search

Lithostratigraphy: Glasford Formation >>Ogle Till Member
Chronostratigraphy: Cenozoic Erathem >>Quaternary System >>Pleistocene Series

Primary source

Willman, H. B., and John C. Frye, 1970, Pleistocene Stratigraphy of Illinois: Illinois State Geological Survey Bulletin 94, 204 p.

Contributing author(s)

H. B. Willman and John C. Frye


Original description

The Ogle Till Member of the Glasford Formation was informally named the Ogle tills (Frye et al., 1969, p. 24). It is herein formally named a member (Willman and Frye 1970).


The Ogle Till Member was informally named the Ogle tills for Ogle County from exposures in western Ogle County (Frye et al., 1969, p. 24).

Other names


Type section

Type location

The Haldane West Section, NE NE NE Sec. 25, T. 24 N., R. 7 E., Ogle County, was designated the type section.

Type author(s)

Type status

Reference section

Reference location

Reference author(s)

Reference status

Stratigraphic relationships

At some places the Ogle Till contains the Sangamon Soil in its top, and at many places it is overlain by Roxana Silt (Lanark Southeast, Lanark West Sections, table 7). At a few places the Ogle Till overlies the Kellerville Till Member, but more commonly it rests on bedrock or on a residual soil developed in bedrock. Further subdivision of the Ogle Member would appear to be appropriate when more data are available.

Extent and thickness

It has been intensely eroded and generally is less than 20 feet thick. The geographic extent of the member is shown in figure 6.


The Ogle tills were described as including three distinctly different till compositions and intercalated outwash of gravel, sand, and silt. Despite its range in mineral composition, the till of the Ogle Member is generally sandy, silty, tan to gray-brown, and interstratified with sand and gravel, characteristics that aid in distinguishing it from the more clayey, gray, compact till of the Sterling Till Member that overlies it. The composition of the Ogle Member is summarized in table 2.




Well log characteristics


Age and correlation

Although a definite age assignment of the Ogle Till has not been made, it is judged to be in the Monican Substage of the Illinoian Stage.

Environments of deposition

Economic importance



FRYE, J. C., H. D. GLASS, J. P. KEMPTON, and H. B. WILLMAN, 1969, Glacial tills of northwestern Illinois: Illinois State Geological Survey Circular 437, 47 p.

ISGS Codes

Stratigraphic Code Geo Unit Designation