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The Nashville Dome of Tennessee and the Jessamine Dome or Lexington Dome [1] 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 Findlay and Kankakee arches. The Findlay plunges under Ontario and reappears as the Algonquin Arch further north. [2]
The Cincinnati Arch was developing across eastern Indiana during the late Ordovician. By the Early Silurian [3] the seas northwest of the Cincinnati Arch began to become shallower. By the Early Mississippian, the Kankakee arch was above sea level. [4] During the Silurian Period (420 to 405 MYA) a shallow sea spread across Indiana. This sea ...
Pointed arches form the rib vaults of Worcester Cathedral (1084–1504) A pointed arch, ogival arch, or Gothic arch is an arch with a pointed crown meet at an angle at the top of the arch. [1] Also known as a two-centred arch, its form is derived from the intersection of two circles. [2]
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 crossing of the Missouri River at Arrow Rock, which was recorded in the 1700s, played an important role in early explorations, such as the Lewis and Clark Expedition in 1804, that led to the opening of the American West. A ferry was later established near Arrow Rock, at what became a starting point for traders on the Santa Fe Trail.
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Geologically, the hill sits in the Dearborn Upland, an area of high terrain in southeast Indiana that sits on top of the geologic structure known as the Cincinnati Arch. However, Hoosier Hill is located in a portion of the upland buried underneath glacial debris known as the Tipton Till Plain. As a result, while the average elevation of this ...
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