Interstate 64 in Kentucky in the context of "Lexington, Kentucky"

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⭐ Core Definition: Interstate 64 in Kentucky

Interstate 64 (I-64) in the US state of Kentucky travels for 191 miles (307 km), passing by the major towns and cities of Louisville, Frankfort, Lexington, and Ashland. It has several major junctions with other Interstates, including I-65, I-71, I-264, and I-265 in Louisville and I-75 in Lexington.

The portion of I-64 in Kentucky is host to two "exceptionally significant" structures indicated by the Federal Highway Administration (FHWA). One is the Cochran Hill Tunnel, a twin tube at Cherokee Park in Louisville built in 1974, and the other is a 1960s-era modern-styled rest area near Winchester.

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Interstate 64 in Kentucky in the context of Ironstone

Ironstone is a sedimentary rock, either deposited directly as a ferruginous sediment or created by chemical replacement, that contains a substantial proportion of an iron ore compound from which iron (Fe) can be smelted commercially.

Not to be confused with native or telluric iron, which is very rare and found in metallic form, the term ironstone is customarily restricted to hard, coarsely banded, non-banded, and non-cherty sedimentary rocks of post-Precambrian age. The Precambrian deposits, which have a different origin, are generally known as banded iron formations. The iron minerals comprising ironstones can consist either of oxides, i.e. limonite, hematite, and magnetite; carbonates, i.e. siderite; silicates, i.e. chamosite; or some combination of these minerals.

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Interstate 64 in Kentucky in the context of Breathitt Formation

The Breathitt Formation is a geologic formation in Kentucky which preserves fossils dating back to the Pennsylvanian period.

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