Age:Mississippian Type designation:Type locality: The name “Waltersburg Sandstone” was proposed by Stuart Weller (1920, p. 398) for exposures of a massive cliff-forming sandstone near Waltersburg, Pope County, Illinois (Gray, 1970, 1986). History of usage:In his initial study of outcropping upper Chesterian rocks in Indiana, Malott (1925, p. 108-109) named a thin ledge-forming sandstone the Wickliffe Sandstone. Later he asserted a correlation with the Waltersburg (Malott, 1931, p. 222), and that name came into general use, replacing Wickliffe (Gray, 1986). Boundaries of the unit were never adequately defined, however (see the discussion of boundary problems under "Tar Springs Formation"), and in a restudy of outcropping upper Chesterian rocks, Gray (1978) did not find need to name a member at this position, which is within the Branchville Formation of surface usage (Gray, 1986). Later, Gray (1986, p. 167) assigned the Waltersburg in Indiana to the Buffalo Wallow Group. Droste and Keller (1995, p. 5) adopted the name “Waltersburg Formation” in the subsurface in Indiana because of the variable lithology of the unit. Description:In Illinois, the Waltersburg is as much as 70 ft (21 m) thick, but it is absent or unrecognizable in many places (Gray, 1986). In discussing the Waltersburg Formation in the standard Chesterian section, Swann (1963, p. 38) described it as primarily dark shale containing elongate sandstone bodies and 35 to 80 ft (11 to 24 m) thick (Gray, 1986).
Boundaries:The Waltersburg Formation overlies the Vienna Limestone or the Tar Springs Formation conformably (Droste and Keller, 1995, p. 7). The formation conformably underlies the Menard Limestone or unconformably underlies strata of the Pennsylvanian System (Droste and Keller, 1995). Economic Importance:Petroleum production: The following petroleum fields have produced oil from the Waltersburg Formation (Mississippian) in Indiana: Belknap, Caborn Consolidated, Caborn West, College Consolidated, Crunk East, Fleener Consolidated, Fleener South, Ford South, Griffin Consolidated, Hatfield, Huesler Consolidated, Inman East, Lamott Consolidated, Martin, Midway Consolidated, Mt. Carmel Consolidated, Mt. Vernon Consolidated, Mt. Vernon South, Mounts, Mumford Hills, Owensville Consolidated, Parker Consolidated, Powells Lake Consolidated, Pueblo, Pueblo East, Rapture, Rapture South, Rochester, Rockport South, Roger East, St. Wendel Consolidated, Springfield Consolidated, Stewartsville South, Sweezer, Vaughn Consolidated, Wadesville North, Welborn Consolidated, West Franklin, and West Hovey (Cazee, 2004). |
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Regional Indiana usage:
Illinois Basin (COSUNA 11)
Misc/Abandoned Names:None Geologic Map Unit Designation:Mw Note: Hansen (1991, p. 52) in Suggestions to authors of the reports of the United States Geological Survey noted that letter symbols for map units are considered to be unique to each geologic map and that adjacent maps do not necessarily need to use the same symbols for the same map unit. Therefore, map unit abbreviations in the Indiana Geologic Names Information System should be regarded simply as recommendations. |
COSUNA areas and regional terminologyNames for geologic units vary across Indiana. The Midwestern Basin and Arches Region COSUNA chart (Shaver, 1984) was developed to strategically document such variations in terminology. The geologic map (below left) is derived from this chart and provides an index to the five defined COSUNA regions in Indiana. The regions are generally based on regional bedrock outcrop patterns and major structural features in Indiana. (Click the maps below to view more detailed maps of COSUNA regions and major structural features in Indiana.) COSUNA areas and numbers that approximate regional bedrock outcrop patterns and major structural features in Indiana. Major tectonic features that affect bedrock geology in Indiana. |
See also:References:Hansen, W. R., 1991, Suggestions to authors of the reports of the United States Geological Survey (7th ed.): Washington, D.C., U.S. Geological Survey, 289 p. Malott, C. A., 1925, The upper Chester of Indiana: Indiana Academy of Science Proceedings, v. 34, p. 103–132. Malott, C. A., 1931, Geologic structure in the Indian and Trinity Springs locality, Martin County, Indiana: Indiana Academy of Science Proceedings, v. 40, p. 217–231. Shaver, R. H., coordinator, 1984, Midwestern basin and arches region–correlation of stratigraphic units in North America (COSUNA): American Association of Petroleum Geologists Correlation Chart Series. Swann, D. H., 1963, Classification of Genevievian and Chesterian (Late Mississippian) rocks of Illinois: Illinois State Geological Survey Report of Investigations 216, 91 p. Weller, Stuart, 1920, The Chester Series in Illinois: Journal of Geology, v. 28, p. 281–303 and 395–416. |
For additional information, contact:
Nancy Hasenmueller (hasenmue@indiana.edu)Date last revised: August 9, 2021