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The State Line Archeological District (also known as the State Line site [1]) is a complex of archaeological sites and national historic district located west of Elizabethtown, Ohio, United States. Located on both sides of the Indiana /Ohio border, [ 2 ] the historic district is composed of five contributing properties spread out across 8 acres ...
Measuring about 5 hectares (12 acres) in area, its name is taken from the area's former use by the Swan family as a landing for riverboats along the Ohio. [ 2 ] : 194 Nearby terrain features include a dirt road at the site's southern end, a large pond just a stone's throw to the south, and the mouth of Indian Creek about 1,800 metres (5,900 ft ...
During the late Mississippian Ohio was covered by a shallow sea. Near the end of the Mississippian the seas withdrew from the state. Ohio was located near the equator. The fossil record of Ohio includes greater numbers of land plants, brachiopods, clams, crinoids, fishes. [4] Ohio was a low-lying swampy plain near the coast during the ...
Free fossil brochure will be provided to all participants. Leaf ID Hike, 2 p.m. at Potato Creek State Park in North Liberty: There are many ways to identify a tree. On this hike, learn how to ...
Fossil formations (Devonian Jeffersonville Limestone) found along the shores of the Ohio River. View of the fossil bed from the overlook. The park includes an interpretive center open to the public. In 1990, the Indiana state government hired Terry Chase, a well-established exhibit developer, to design the center's displays.
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Indiana Geological Survey page on Jeffersonville Limestone KYANA Geological Society Devonian page , showing photographs of fossils collected from the Jeffersonville and other formations guidebook Silurian and Devonian Geology and Paleontology at the Falls of the Ohio, Kentucky/Indiana , 42nd Annual Meeting of the American Institute of ...
An early map of the Falls of the Ohio; Louisville, Kentucky is in the lower right The area is located at the Falls of the Ohio, which was the only navigational barrier on the river in earlier times. The falls were a series of rapids formed by the relatively recent erosion of the Ohio River operating on 386-million-year-old Devonian hard ...