Cincinnati Arch

rdf:langString Cincinnati Arch

rdf:langString The Cincinnati Arch is a broad structural uplift between the Illinois Basin to the west, the Michigan Basin to the northwest and the Appalachian Basin and Black Warrior Basin to the east and southeast. It existed as a positive topographic area during Late Ordovician through the Devonian Period which stretched from northern Alabama northeastward to the southeastern tip of Ontario. Fossils from the Ordovician Period are commonplace in the geologic formations which make up the Cincinnati Arch, and are commonly studied along man made roadcuts. The Nashville Dome of Tennessee and the Jessamine Dome or of central Kentucky make up the central portion of the Arch. In the northern part, north of Cincinnati, Ohio, the Cincinnati Arch branches to form the and Kankakee arches. The Findlay plunges under Ontario and reappears as the further north. Petroleum was first discovered in a relatively low part of the arch, between the Jessamine and Nashville domes, the Cumberland Saddle, in Cumberland County, Kentucky in 1829. The Saddle and adjoining areas have been significant producers since drilling for oil came to the region in the late 1800s.