Age:Mississippian Type designation:Type locality: The name "Fredonia" was originally applied to rocks exposed near Fredonia, Caldwell County, Kentucky, by Ulrich and Smith (1905, p. 24, 39, 40) (Smith, 1970; Carr and Gray, 1986). History of usage:Extended: The term was first applied in Indiana by Cumings (1922, p. 507), who suggested that the Paoli Limestone, which then included all of what is now called the Ste. Genevieve as well as the present Paoli (Elrod, 1899, p. 259), was equivalent to the type Fredonia (Carr and Gray, 1986).
Description:The Fredonia Member in Indiana consists dominantly of an assortment of light-colored carbonate rocks that may have a few shale partings and interbedded carbonate rocks with shale beds as much as 10 ft (3 m) thick (Droste and Carpenter, 1990). The porous zones in the Fredonia are generally oolitic or biofragmental limestones or very dolomitic limestones or dolostone. The units are lens shaped and laterally discontinuous (Droste and Carpenter, 1990).
Correlations:The revised Fredonia of Droste and Carpenter (1990) is equivalent to both the Fredonia Limestone and the Spar Mountain Sandstone Members of the Ste. Genevieve Limestone of Illinois. |
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Regional Indiana usage:
Illinois Basin (COSUNA 11)
Misc/Abandoned Names:Horse Cave Member (of the St. Louis Limestone), Spar Mountain Member Geologic Map Unit Designation:Msgf 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. |
References:Cumings, E. R., 1922, Nomenclature and description of the geological formations of Indiana, in Logan, W. N., Cumings, E. R., Malott, C. A., Visher, S. S., Tucker, W. M., Reeves, J. R., and Legge, H. W., Handbook of Indiana geology: Indiana Department of Conservation Publication No. 21, pt. 4, p. 403–570. Elrod, M. N., 1899, The geologic relations of some St. Louis Group caves and sinkholes: Indiana Academy of Science Proceedings for 1898, p. 258–267. 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., 1945, Rosiclare and Aux Vases Sandstones in southern Indiana [abs.]: Geological Society of America Bulletin, v. 56, p. 1,180. Malott, C. A., 1946, The geology of Cataract Falls, Owen County, Indiana: Journal of Geology, v. 54, p. 322–326. Malott, C. A., 1952, Stratigraphy of the Ste. Genevieve and Chester formations of southern Indiana: Ann Arbor, Michigan, Edwards Letter Shop, 105 p. 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. Ulrich, E. O., and Smith, W. S. T., 1905, The lead, zinc, and fluorspar deposits of western Kentucky U.S. Geological Survey Professional Paper 36, 218 p. |
For additional information, contact:
Nancy Hasenmueller (hasenmue@indiana.edu)Date last revised: May 27, 2016