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From Wikipedia, the free encyclopedia

This article is about a United States mountain pass. For other uses, see Cumberland Gap (disambiguation).
Cumberland Gap

Cumberland Gap in winter
Elevation 1600 ft./488 m.
Traversed by U.S. Highway 25E
Location Kentucky/Virginia/Tennessee,  United States
Range Cumberland Mountains
Coordinates 36°36′14″N 83°40′27″W / 36.6038°N 83.6742°W / 36.6038; -83.6742Coordinates: 36°36′14″N 83°40′27″W / 36.6038°N 83.6742°W / 36.6038; -83.6742
Daniel Boone Escorting Settlers through the Cumberland Gap (George Caleb Bingham, oil on canvas, 1851–52)

Cumberland Gap (el. 1600 ft./488 m.) is a pass through the Cumberland Mountains region of the Appalachian Mountains, also known as the Cumberland Water Gap, at the juncture of the U.S. states of Tennessee, Kentucky, and Virginia. Famous in American history for its role as one key passageway through the lower central Appalachians, it was an important part of the Wilderness Road and is now part of the Cumberland Gap National Historical Park. The Cumberland Gap was discovered in 1750 by Dr. Thomas Walker, a Virginia physician and explorer. Long used by Native Americans, the path was widened by a team of loggers led by Daniel Boone, making it accessible to pioneers, who used it to journey into the western frontiers of Kentucky and Tennessee.



Cumberland Gap is located just north of the spot where the current-day states of Kentucky, Tennessee, and Virginia meet. The nearby town of Cumberland Gap, Tennessee takes its name from the pass.

The gap was formed by an ancient creek, flowing southward, which cut through the land being pushed up to form the mountains. As the land rose even more, the creek reversed direction flowing into the Cumberland River to the north. The gap was used by Native Americans and migrating animal herds.


Map showing Cumberland Gap in relation to the Wilderness Road route from Virginia to Kentucky

The gap was named for Prince William Augustus, Duke of Cumberland, who had many places named for him in the American colonies after the Battle of Culloden. The explorer Thomas Walker gave the name to the Cumberland River in 1750, and the name soon spread to many other features in the region, such as the Cumberland Gap. In 1769 Joseph Martin built a fort nearby at present-day Rose Hill, Virginia, on behalf of Dr. Walker's land claimants. But Martin and his men were chased out of the area by Native Americans, and Martin himself did not return until 1775.[1]

In 1775, Daniel Boone, hired by the Transylvania Company, arrived in the region, leading a company of men to widen the path through the gap to make settlement of Kentucky and Tennessee easier. On his arrival, Boone discovered that Martin had beaten him to Powell Valley, where Martin and his men were clearing land for their own settlement – the westernmost settlement in English colonial America at the time.[2] By the 1790's the trail that Boone and his men built was widened to accommodate wagon traffic.

It is estimated that between 200,000 and 300,000 immigrants passed through the gap on their way into Kentucky and the Ohio Valley before 1810. Today 18,000 cars pass beneath the site daily, and 1,200,000 people visit the park on the site annually.[3]

U.S. Route 25E passed overland through the gap before the completion of the Cumberland Gap Tunnel in 1996. The original trail was then restored.

Joseph Martin, explorer, long hunter, and later general

Historic district

The gap and associated historic resources were listed on the National Register of Historic Places as a historic district on May 28, 1980.[4]

Geological features

The 12-mile (19 km) long Cumberland Gap consists of four geologic features: the Yellow Creek valley, the natural gap in the Cumberland Mountain ridge, the eroded gap in the Pine Mountain, and Middlesboro crater.

Middlesboro crater is a 3-mile (4.8 km) diameter meteorite impact crater in which Middlesboro, Kentucky is located. The crater was identified in 1966 when Robert Dietz discovered shatter cones in sandstone, which led to the further identification of shocked quartz. Shatter cones, a rock shattering pattern naturally formed only during impact events, are found in abundance in the area. In September 2003 the site was designated a Distinguished Geologic Site by the Kentucky Society of Professional Geologists.[citation needed]

Without Middlesboro crater, it would have been difficult for packhorses to navigate this gap and improbable that wagon roads would have been constructed at an early date. Middlesboro is the only place in the world where coal is mined inside an impact crater. Special mining techniques must be used in the complicated strata of this crater. (Milam & Kuehn, 36).

Panoramic view from Pinnacle Overlook at Cumberland Gap National Historic Park

References in popular culture

See also


  1. ^ A Cumberland Gap Area Guidebook, Tom N. Shattuck, The Wilderness Road Company, 1999, ISBN 978-0-9677765-3-8
  2. ^ Boone: A Biography, Robert Morgan, Algonquin Books, Chapel Hill, ISBN 978-1-56512-455-4
  3. ^ "Cumberland Gap". 
  4. ^ National Register of Historic Places Nomination Form: Cumberland Gap Historic District - Virginia/Kentucky/Tennessee, 1980

External links


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