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The St. Louis Limestone is a large geologic formation covering a wide area of the midwest of the United States. It is named after an exposure at St. Louis, Missouri . It consists of sedimentary limestone with scattered chert beds, including the heavily chertified Lost River Chert Bed in the Horse Cave Member .
The Plattin Limestone is a Middle Ordovician geologic formation in Arkansas, Illinois, and Missouri. [1] The name was first introduced in 1904 by Edward Oscar Ulrich in his study of the geology of Missouri. [2] A type locality was designated at the mouth of the Plattin Creek in Jefferson County, Missouri, however a stratotype was not assigned ...
Owens Quarry, a limestone quarry and crusher plant near Marion, Ohio, around which the community of Owens, Ohio grew. Ridgeway Site, in Hardin County, Ohio, a former archaeological site which, during excavation of its gravel, yielded numerous artifacts and buried bodies of the Glacial Kame culture, for which it is the type site.
Includes a limestone quarry and kilns for producing quicklime, built in 1911 and abandoned in the 1920s. William Johnston Lime Kiln, Saylesville, Wisconsin, NRHP-listed; Hadfield Company Lime Kilns, Waukesha, Wisconsin, NRHP-listed; List of historical markers in Kewaunee County, Wisconsin; Limekiln State Park, Big Sur, California; Quarry ...
World-wide distribution of MVT deposits (red), clastic sediment-hosted (green), and unclassified (blue) lead-zinc deposits. Source: USGS. Carbonate-hosted lead-zinc ore deposits are important and highly valuable concentrations of lead and zinc sulfide ores hosted within carbonate (limestone, marl, dolomite) formations and which share a common genetic origin.
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In 1904, the Missouri Bureau of Geology named Phenix as the largest and best equipped quarry in the state with a community of 500 employees. [ 5 ] During the first three decades of the 20th century, Phenix Marble Company was one of the largest producers of cut limestone and marble west of the Mississippi, producing more than 250,000 cubic feet ...
The Ste. Genevieve Limestone is a geologic formation named for Ste. Genevieve, Missouri where it is exposed and was first described. It is a thick-bedded limestone that overlies the St. Louis Limestone. Both are Mississippian in age. The St. Louis Limestone is Meramecian and the Ste. Genevieve is the base of the Chesterian series. [1]