Difference between revisions of "Winnebago Formation"

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==Primary source==
 
==Primary source==
Willman, H. B., and John C. Frye, 1970, Pleistocene Stratigraphy of Illinois: Illinois State Geological Survey Bulletin 94, 204 p.
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Willman, H. B., and John C. Frye, 1970, Pleistocene Stratigraphy of Illinois: Illinois State Geological Survey Bulletin 94, 204 p.<br>
 +
 
 +
---<br>
 +
Berg, R.C., J. P. Kempton, L. R. Follmer, D. P. McKenna, 1985, Illinoian and Wisconsinan stratigraphy and environments in northern Illinois: the Altonian revised: Illinois State Geological Survey Guidebook 19, 177 pp.
 +
 
 +
Berg R. C., E. D. McKay III, R. J. Goble, and H. Wang, 2013, Age of the Winnebago Formation of north-central Illinois as determined by optically stimulated luminescence dating: Illinois State Geological Survey Circular 580, 15 p. 
 +
 
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Curry, B. B., 1989, Absence of Altonian glaciation in Illinois: Quaternary Research 31, p. 1–13.
 +
 
 +
Hansel, A. K., E. D. McKay III, 2010, Quaternary period, ''in'' Kolata, D. R., and C. K. Nimz, (Eds.), Geology of Illinois. Illinois State Geological Survey, Champaign, IL, pp. 216–247.
  
 
==Contributing author&#40;s&#41;==
 
==Contributing author&#40;s&#41;==
H. B. Willman and John C. Frye
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H. B. Willman and John C. Frye, David A. Grimley
  
 
==Name==
 
==Name==
  
 
===Original description===
 
===Original description===
The Winnebago Formation was informally named Winnebago drift (Frye and Willman, 1960) for Winnebago County, as a replacement for the term Farmdale drift (Shaffer, 1956). The term was formalized as a formation in 1969 (Frye et al.).
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The Winnebago Formation was informally named Winnebago drift (Frye and Willman, 1960) for Winnebago County, as a replacement for the term Farmdale drift (Shaffer, 1956). The term was formalized as a formation in 1969 (Frye et al.).<br>
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The unit is now considered to be late Illinois Episode (Berg et al., 1985; Curry; 1989; Hansel and McKay, 2010)
  
 
===Derivation===
 
===Derivation===
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==Stratigraphic relationships==
 
==Stratigraphic relationships==
The formation was defined to include those glacial deposits bounded by the Farmdale Soil at the top and the Sangamon Soil at the base.<br>
+
The formation was originally defined to include those glacial deposits bounded by the Farmdale Soil at the top and the Sangamon Soil at the base. However, the Sangamon Geosol is now known to occur stratigraphically above the Winnebago Formation (but is largely eroded due to periglacial processes).<br>
  
It is subdivided into three named members: the Capron Till Member at the top, the Plano Silt Member below the Capron, and the Argyle Till Member below the Plano Silt. In the
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The Winnebago Formation was originally subdivided into three named members: the Capron Till Member at the top, the Plano Silt Member (note: this unit now abandoned; Curry, 1989) below the Capron, and the Argyle Till Member below. In the subsurface below the Argyle are silts, tills, and some outwash that have not been differentiated into members.
subsurface below the Argyle are silts, tills, and some outwash that have not been differentiated into members. The spatial relation of the Winnebago to adjacent stratigraphic units is shown diagrammatically in figure 8.
 
 
 
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{| class="wikitable" style="text-align: center;"
 
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|<gallery caption="" widths=250px heights=250px perrow=4>
 
94-fig_8.jpg|{{file:94-fig_8.jpg}}
 
</gallery>
 
|}
 
</center>
 
  
 
==Extent and thickness==
 
==Extent and thickness==
In the type section the Winnebago consists of 1.5 feet of Peoria Loess overlying 6 feet of leached till and 7 feet of calcareous, pink, sandy and cobbly till. The till is the Argyle Till Member of the Winnebago Formation. The Winnebago Formation probably is as much as 400 feet thick in the deeper bedrock valleys. The geographic distribution of the formation at the surface is indicated on the map in figure 6.
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In the type section the Winnebago consists of 1.5 feet of Peoria Loess overlying 6 feet of leached till and 7 feet of calcareous, pink, sandy and cobbly till. The till is the Argyle Till Member of the Winnebago Formation. The Winnebago Formation probably is as much as 400 feet thick in the deeper bedrock valleys. This unit occurs in Boone and Winnebago Counties of north-central Illinois.
 
 
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{| class="wikitable" style="text-align: center;"
 
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</center>
 
  
 
==Lithology==
 
==Lithology==
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==Age and correlation==
 
==Age and correlation==
Radiocarbon dates determined from the formation are listed in table 1. <br>
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The Winnebago Formation was originally interpreted to have been deposited within the Altonian Substage of the Wisconsinan Stage (Willman and Frye, 1970).  However, it is now interpreted to have been deposited during later phases of the Illinois Episode (Berg et al., 1985; Curry, 1989; Hansel and McKay, 2010; Berg et al., 2013). The occurrence of the Sangamon Geosol developed into the Winnebago Formation is patchy because of periglacial erosion during the last glaciation. Deposition of the Winnebago Formation is largely related largely to glacial advances from the Lake Michigan Lobe and possibly the Green Bay Lobe (Berg et al., 2013).
 
 
<center>
 
{| class="wikitable" style="text-align: center;"
 
|-
 
|<gallery caption="" widths=250px heights=250px perrow=4>
 
94-tb_1.jpg|{{file:94-tb_1.jpg}}
 
</gallery>
 
|}
 
</center>
 
 
 
The Winnebago Formation is entirely within the Altonian Substage of the Wisconsinan Stage. It is related largely to glacial advances from the Lake Michigan Lobe and possibly the Green Bay Lobe.
 
  
 
==Environments of deposition==
 
==Environments of deposition==
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==References==
 
==References==
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.<br>
+
* Berg, R.C., J. P. Kempton, L. R. Follmer, D. P. McKenna, 1985, Illinoian and Wisconsinan stratigraphy and environments in northern Illinois: the Altonian revised: Illinois State Geological Survey, Guidebook 19, 177 p.<br>
FRYE, J. C., and H. B. WILLMAN, 1960, Classification of the Wisconsinan Stage in the Lake Michigan Glacial Lobe: Illinois State Geological Survey Circular 285, 16 p.<br>
+
* Berg R. C., E. D. McKay III, R. J. Goble, and H. Wang, 2013, Age of the Winnebago Formation of north-central Illinois as determined by optically stimulated luminescence dating: Illinois State Geological Survey, Circular 580, 15 p.<br>
FRYE, J. C., and H. B. WILLMAN, 1965a, [Illinois part of] Guidebook for field conference C—Upper Mississippi Valley (R. P. Goldthwait [organizer]; C. B. Schultz and H. T. U.  
+
* Curry, B. B., 1989, Absence of Altonian glaciation in Illinois: Quaternary Research 31, p. 1–13.<br>
Smith [eds.]): International Association of Quaternary Research 7th Congress, Nebraska Academy of Science, p. 81-110; Illinois State Geological Survey Reprint 1966-B (supplemental data, J. P. Kempton and H. D. Glass, p. C-S1-C-S11), 41 p.<br>
+
* 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.<br>
KEMPTON, J. P., 1963, Subsurface Stratigraphy of Pleistocene Deposits of Central-Northern Illinois: Illinois State Geological Survey Circular 356, 43 p.<br>
+
* Frye, J. C., and H. B. Willman, 1960, Classification of the Wisconsinan Stage in the Lake Michigan Glacial Lobe: Illinois State Geological Survey, Circular 285, 16 p.<br>
SHAFFER, P. R., 1956, Farmdale drift in northwestern Illinois: Illinois State Geological Survey Report of Investigations 198, 25 p.<br>
+
* Frye, J. C., and H. B. Willman, 1965a, [Illinois part of] Guidebook for field conference C—Upper Mississippi Valley (R. P. Goldthwait [organizer]; C. B. Schultz and H. T. U. Smith [eds.]): International Association of Quaternary Research 7th Congress, Nebraska Academy of Science, p. 81-110; Illinois State Geological Survey Reprint 1966-B (supplemental data, J. P. Kempton and H. D. Glass, p. C-S1-C-S11), 41 p.<br>
 +
* Hansel, A. K., E. D. McKay III, 2010, Quaternary period, in Kolata, D. R., and C. K. Nimz, (Eds.), Geology of Illinois. Illinois State Geological Survey, Champaign, IL, pp. 216–247.<br>
 +
* Kemption, J. P., 1963, Subsurface Stratigraphy of Pleistocene Deposits of Central-Northern Illinois: Illinois State Geological Survey, Circular 356, 43 p.<br>
 +
* Shaffer, P. R., 1956, Farmdale drift in northwestern Illinois: Illinois State Geological Survey, Report of Investigations 198, 25 p.<br>
  
 
{{Codes
 
{{Codes

Latest revision as of 14:34, 12 October 2018

Lithostratigraphy: Winnebago Formation
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.

---
Berg, R.C., J. P. Kempton, L. R. Follmer, D. P. McKenna, 1985, Illinoian and Wisconsinan stratigraphy and environments in northern Illinois: the Altonian revised: Illinois State Geological Survey Guidebook 19, 177 pp.

Berg R. C., E. D. McKay III, R. J. Goble, and H. Wang, 2013, Age of the Winnebago Formation of north-central Illinois as determined by optically stimulated luminescence dating: Illinois State Geological Survey Circular 580, 15 p.

Curry, B. B., 1989, Absence of Altonian glaciation in Illinois: Quaternary Research 31, p. 1–13.

Hansel, A. K., E. D. McKay III, 2010, Quaternary period, in Kolata, D. R., and C. K. Nimz, (Eds.), Geology of Illinois. Illinois State Geological Survey, Champaign, IL, pp. 216–247.

Contributing author(s)

H. B. Willman and John C. Frye, David A. Grimley

Name

Original description

The Winnebago Formation was informally named Winnebago drift (Frye and Willman, 1960) for Winnebago County, as a replacement for the term Farmdale drift (Shaffer, 1956). The term was formalized as a formation in 1969 (Frye et al.).

The unit is now considered to be late Illinois Episode (Berg et al., 1985; Curry; 1989; Hansel and McKay, 2010)

Derivation

Other names

History/background

Type section

Type location

The type locality was designated as the Rock Valley College Section and adjacent exposures and Northwest Tollway borings No. 2 and No. 5 (Kempton, 1963, p. 38). The type section is in the Rock Valley College Section, SW NW SW Sec. 10, T. 44 N., R. 2 E.

Type author(s)

Type status

Reference section

Reference location

Reference author(s)

Reference status

Stratigraphic relationships

The formation was originally defined to include those glacial deposits bounded by the Farmdale Soil at the top and the Sangamon Soil at the base. However, the Sangamon Geosol is now known to occur stratigraphically above the Winnebago Formation (but is largely eroded due to periglacial processes).

The Winnebago Formation was originally subdivided into three named members: the Capron Till Member at the top, the Plano Silt Member (note: this unit now abandoned; Curry, 1989) below the Capron, and the Argyle Till Member below. In the subsurface below the Argyle are silts, tills, and some outwash that have not been differentiated into members.

Extent and thickness

In the type section the Winnebago consists of 1.5 feet of Peoria Loess overlying 6 feet of leached till and 7 feet of calcareous, pink, sandy and cobbly till. The till is the Argyle Till Member of the Winnebago Formation. The Winnebago Formation probably is as much as 400 feet thick in the deeper bedrock valleys. This unit occurs in Boone and Winnebago Counties of north-central Illinois.

Lithology

The Winnebago Formation consists of tills, silts, peats, and outwash. The formation has been described in detail from deep core borings in Kane and McHenry Counties (Kempton, in Frye and Willman, 1965a), and its textural and mineral composition has been described (Frye et al., 1969).

Compositional data are given in tables 2, 4, and 5.

Core(s)

Photograph(s)

Contacts

Well log characteristics

Fossils

Age and correlation

The Winnebago Formation was originally interpreted to have been deposited within the Altonian Substage of the Wisconsinan Stage (Willman and Frye, 1970). However, it is now interpreted to have been deposited during later phases of the Illinois Episode (Berg et al., 1985; Curry, 1989; Hansel and McKay, 2010; Berg et al., 2013). The occurrence of the Sangamon Geosol developed into the Winnebago Formation is patchy because of periglacial erosion during the last glaciation. Deposition of the Winnebago Formation is largely related largely to glacial advances from the Lake Michigan Lobe and possibly the Green Bay Lobe (Berg et al., 2013).

Environments of deposition

Economic importance

Remarks

References

  • Berg, R.C., J. P. Kempton, L. R. Follmer, D. P. McKenna, 1985, Illinoian and Wisconsinan stratigraphy and environments in northern Illinois: the Altonian revised: Illinois State Geological Survey, Guidebook 19, 177 p.
  • Berg R. C., E. D. McKay III, R. J. Goble, and H. Wang, 2013, Age of the Winnebago Formation of north-central Illinois as determined by optically stimulated luminescence dating: Illinois State Geological Survey, Circular 580, 15 p.
  • Curry, B. B., 1989, Absence of Altonian glaciation in Illinois: Quaternary Research 31, p. 1–13.
  • 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.
  • Frye, J. C., and H. B. Willman, 1960, Classification of the Wisconsinan Stage in the Lake Michigan Glacial Lobe: Illinois State Geological Survey, Circular 285, 16 p.
  • Frye, J. C., and H. B. Willman, 1965a, [Illinois part of] Guidebook for field conference C—Upper Mississippi Valley (R. P. Goldthwait [organizer]; C. B. Schultz and H. T. U. Smith [eds.]): International Association of Quaternary Research 7th Congress, Nebraska Academy of Science, p. 81-110; Illinois State Geological Survey Reprint 1966-B (supplemental data, J. P. Kempton and H. D. Glass, p. C-S1-C-S11), 41 p.
  • Hansel, A. K., E. D. McKay III, 2010, Quaternary period, in Kolata, D. R., and C. K. Nimz, (Eds.), Geology of Illinois. Illinois State Geological Survey, Champaign, IL, pp. 216–247.
  • Kemption, J. P., 1963, Subsurface Stratigraphy of Pleistocene Deposits of Central-Northern Illinois: Illinois State Geological Survey, Circular 356, 43 p.
  • Shaffer, P. R., 1956, Farmdale drift in northwestern Illinois: Illinois State Geological Survey, Report of Investigations 198, 25 p.

ISGS Codes

Stratigraphic Code Geo Unit Designation
0640
wi