Everything about Cumberland Gap totally explained
» "Cumberland Gap" is also the informal name for a section of the A74 in England; the name of a song by skiffle artist Lonnie Donegan; and the name of an old-time fiddle tune with many variants.
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. Famous in American history for its role as the chief passageway through the central Appalachians, it was an important part of the
Wilderness Road. Long used by Native Americans, the path was made more accessible for pioneer travel when
Daniel Boone used 35 axmen to widen it. Due to his work, pioneers could use wagons to journey into the western frontiers of Kentucky and Tennessee.
Location
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.
History
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 1775,
Daniel Boone, hired by the
Transylvania Company led a company of men to widen the path through the gap to make settlement of Kentucky and Tennessee easier. The trail was widened in the 1790s 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.
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.
Geological features
The 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 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.
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).
References in popular culture
Further Information
Get more info on 'Cumberland Gap'.
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