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The Kentucky River is a tributary of the Ohio River in Kentucky, United States. The 260-mile (420 km) river and its tributaries drain much of eastern and central Kentucky, passing through the Eastern Coalfield, the Cumberland Mountains, and the Bluegrass region. [2] Its watershed encompasses about 7,000 square miles (18,000 km 2), and it ...
Kentucky is the only U.S. state to have a continuous border of rivers running along three of its sides – the Mississippi River to the west, the Ohio River to the north, and the Big Sandy River and Tug Fork to the east. [30] Its major internal rivers include the Kentucky River, Tennessee River, Cumberland River, Green River and Licking River.
The river cuts a deep canyon called the Kentucky River Palisades through the region, preserving meanders that indicate that the river was once a mature low valley that was suddenly uplifted. Particularly near the Kentucky River, the region exhibits Karst topography, with sinkholes, caves, and disappearing streams that drain underground to the ...
The geology of Kentucky formed beginning more than one billion years ago, in the Proterozoic eon of the Precambrian. The oldest igneous and metamorphic crystalline basement rock is part of the Grenville Province, a small continent that collided with the early North American continent. The beginning of the Paleozoic is poorly attested and the ...
Sinking Creek (Jessamine County, Kentucky) South Fork Kentucky River. Squabble Creek. Tearcoat Creek. Tennessee River. Tradewater River. Tug Fork of the Big Sandy River. Tygarts Creek. Wolf River.
The Kentucky River Palisades is a cliff-lined entrenched meander.The meanders originally formed on the Lexington Peneplain.As sea-level lowered during the Quaternary Period, base level lowered and the meander-form river eroded downward into Ordovician-age limestones, shales, and dolomites in the Central Bluegrass Region.
The Licking River is a partly navigable, 303-mile-long (488 km) [2] tributary of the Ohio River in northeastern Kentucky.The river and its tributaries drain much of the region of northeastern Kentucky between the watersheds of the Kentucky River to the west and the Big Sandy River to the east.
The Cumberland Plateau is a deeply dissected plateau, with topographic relief commonly of about 400 feet (120 metres), and frequent sandstone outcroppings and bluffs.. At Kentucky's Pottsville Escarpment, which is the transition from the Cumberland Plateau to the Bluegrass in the north and the Pennyrile in the south, there are many spectacular cliffs, gorges, rockhouses, natural bridges, and ...