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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 .
Indiana is the Limestone Capital of the world. Many quarries are located in southern Indiana, including The Empire Quarry, which supplied stone for The Empire State Building. Oolitic Indiana is home to Indiana Limestone Corporation, the longest operating stone quarry in the United States.
SubTropolis is a business complex located inside of a 55,000,000-square-foot (5,100,000 m 2), 1,260-acre (5.1 km 2) mine in the bluffs north of the Missouri River in Kansas City, Missouri, United States.
The St. Clair Limestone is a geologic unit in Arkansas, and Oklahoma. It is classified as a Geologic Member in Indiana and Missouri. It is classified as a Geologic Member in Indiana and Missouri. It dates back to the Middle of Silurian period .
The following are approximate tallies of current listings by county. These counts are based on entries in the National Register Information Database as of March 13, 2009 [2] and new weekly listings posted since then on the National Register of Historic Places web site. [3]
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]
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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 ...
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