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Wabaunsee Group

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Geologic group in Kansas, United States
Wabaunsee Group
Stratigraphic range: Gzhelian PreꞒ O S D C P T J K Pg N ↓ (Virgilian stage)
TypeGroup
Unit ofVirgilian series
Sub-units
UnderliesAdmire Group
OverliesShawnee Group
Lithology
PrimaryCyclothems of limestone and shale
OtherMudstone, sand, coal
Location
RegionKansas
CountryUnited States
Type section
Named forWabaunsee County, Kansas
Named byC.S. Prosser
Year defined1895

The Wabaunsee Group is a Late-Carboniferous geologic group in Kansas, extending into Nebraska, Iowa, Missouri, and Oklahoma. The unit is recognized in the subsurface by drillers in Colorado as Wabaunsee Formation.

In locations, some upper members are not present due to a series of erosions that occurred in late-Pennsylvanian time.

See also

References

  1. ^ P. H. Heckel (2013). "Pennsylvanian stratigraphy of Northern Midcontinent Shelf and biostratigraphic correlation of cyclothems". Stratigraphy. 10 (1–2): 7, TEXT-FIGURE 4. Retrieved 2024-06-02.
  2. ^ "Geologic Unit: Wabaunsee". National Geologic Database. Geolex — Significant Publications. United States Geological Survey. Retrieved 2024-06-02. "The formation covers one-half of Wabaunsee County and, on account of the excellent exposures along nearly every stream in the eastern and northern portions of the county, I would propose that it be called the Wabaunsee formation" (Prosser, 1895, p. 689-690).
  3. Jewett, John M. (1941). The Geology of Riley and Geary Counties, Kansas, Kansas Geological Survey Bulletin 39. University of Kansas Publications, Kansas Geological Survey. The upper portion of the Auburn Shale is the lowest stratigraphic unit exposed in Riley County, and the Pennsylvanian strata above the Dover limestone have almost everywhere been removed by erosion that occurred at the end of Pennsylvanian time or they are now concealed by younger deposits, especially by Recent alluvium.
  4. Classification of Rock in Kansas, Kansas Geological Survey, 1986 (Revised November 2018).
    Note: The chart illustrates the series of erosions beginning within the Willard Shale.
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