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Markham Silt Member

From ILSTRAT

Lithostratigraphy: Roxana Silt >>Markham Silt 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

Name

Original description

Markham Silt Member (Willman and Frye 1970).

Derivation

The Markham Silt Member is named for Markham, a village on the Norfolk and Western Railroad 4 miles west of Jacksonville, Morgan County.

Other names

The Markham Member previously was called Roxana Zone la (Frye and Willman, 1963b). It is the same as "upper story Sangamon" in recent Iowa literature (Ruhe et al., 1968).

History/background

Type section

Type location

Its type section is the Chapin Section (table 6) in roadcuts along Illinois Highway 104, 1.5 miles northwest of Markham, on the west side of Mauvaise Terre Creek, SW NE NW Sec. 8, T. 15 N., R. 11 W.

Table 6 -- Stratigraphic Sections (partial)
The following stratigraphic sections describe exposures in Illinois and illustrate many aspects of Pleistocene stratigraphy, including type localities and analytical sample data.

Type author(s)

Type status

Reference section

Reference location

Reference author(s)

Reference status

Stratigraphic relationships

Its spatial relations are shown in figure 8.

Extent and thickness

Lithology

In many places the Markham is a colluvium of silt and some sand with small pebbles, and locally it is entirely within the A-zone and B-zone of the Chapin Soil. Along the Illinois River Valley it commonly contains some loess admixed with the colluvium, and so has a mineral composition different from that of the underlying Sangamon Soil (Frye, Glass, and Willman, 1962; Glass, in Frye and Willman, 1965b), but along the Mississippi River Valley its mineral composition is commonly indistinguishable from that of the underlying Sangamon Soil B-zone. Other stratigraphic sections with this report describing the Markham Member are the Campbells Hump, Cottonwood School, Gale, Jubilee College, and Tindall School Sections (table 6). Its mineral composition is given in table 5.

Table 6 -- Stratigraphic Sections (partial)

Selected analyses from stratigraphic sections (X-ray analyses by Illinois State Geological Survey).

Core(s)

Photograph(s)

Contacts

Well log characteristics

Fossils

Age and correlation

The Markham Member is in the earliest part of the Altonian Substage of the Wisconsinan Stage.

Environments of deposition

Economic importance

Remarks

References

FRYE, J. C, H. D. GLASS, and H. B. WILLMAN, 1962, Stratigraphy and mineralogy of the Wisconsinan loesses of Illinois: Illinois State Geological Survey Circular 334, 55 p.
FRYE, J. C, and H. B. WILLMAN, 1963b, Loess stratigraphy, Wisconsinan classification and accretion-gleys in central western Illinois: Midwestern Section Friends of the Pleistocene, 14th Annual Meeting, Illinois State Geological Survey Guidebook Series 5, 37 p.
FRYE, J. C, and H. B. WILLMAN, 1965b, Illinois, in Guidebook for field conference G— Great Lakes- Ohio River Valley (R. F. Black and E. C. Reed [organizers]; C. B. Schultz and H. T. U. Smith [eds.]): International Association of Quaternary Research 7th Congress, Nebraska Academy of Science, p. 5-26; Illinois State Geological Survey Reprint 1966-B (supplemental data, H. D. Glass, p. G-S1 - G-S4), 26 p.
RUHE, R. V. (et al.), W. P. DIETZ, T. E. FENTON, and G. F. HALL, 1968, Iowan drift problem, northeastern Iowa: Iowa Geological Survey Report of Investigations 7, 40 p.

ISGS Codes

ISGS Code and Symbol
Stratigraphic Code Geo Unit Designation

0710

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