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Matthews Stone Company Historic District is a national historic district located in Richland Township, Monroe County, Indiana.The district encompasses five contributing buildings, one contributing site, six contributing structures, and two contributing objects associated with the Matthews Brothers Stone Company limestone business, now operated as Bybee Stone Company, Inc.
The St Clair is designated as a member of the Bainbridge Group in the State of Indiana. [5] In Illinois, Missouri, Arkansas and Oklahoma it is part of the Hunton Megagroup. The St. Clair is the Basal member of the Niagaran Series, making it part of the Tippecanoe sequence. Throughout most of the Southern extent the unit is roughly 10 to 20' thick.
Burlington Limestone is present in nearly all major Mississippian outcrop regions in Missouri. It is known from Iowa to northwestern Arkansas and from western Illinois to western Kansas . It is present throughout Missouri, except in the Ozark uplift, where it has been removed by erosion .
It is located on the banks of the Ohio River at Clarksville, Indiana, across from Louisville, Kentucky. The park is part of the Falls of the Ohio National Wildlife Conservation Area. The exposed fossil beds of the Jeffersonville Limestone dated from the Devonian period are the main feature of the park, attracting about 160,000 visitors annually ...
The Paoli Formation, Paoli Limestone, or Paoli Chert is a geologic formation in Indiana, Illinois, Kentucky and Missouri. This formation contains members that are known hydrocarbon reservoirs . [ 1 ]
The Salem Formation is a geologic formation in Illinois, Indiana, Kentucky, and Missouri. It preserves fossils dating back to the Mississippian subperiod . This formation is quarried and used as a building material, known as " Indiana limestone ", also called Bedford limestone.
Outcrops along Davis Creek, St. Francois County, Missouri The Davis Formation is a geologic formation in Indiana and Missouri . It preserves fossils dating back to the Cambrian period .
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]