The Middlesboro crater (or astrobleme) is a meteorite crater in Kentucky, United States. It is named after the city of Middlesborough (both spellings are used), which today occupies much of the crater.
The city of Middlesboro is built within the crater
|Diameter||6 kilometers (3.7 mi)|
Permian to late Mesozoic
|Location||Bell County, Kentucky, United States|
|Access||U.S. Route 25E|
The crater is approximately 3 miles (about 5 km) wide and its age is estimated to be less than 300 million years (Permian). The impactor is estimated to have been about 100 m in diameter.
The Middlesboro crater is located in the Appalachian Mountains, between the Cumberland Mountains and Pine Mountain. It forms part of the string of geological features that made the Cumberland Gap a critical westward passage during the settlement of Kentucky and the Ohio Valley in the late 18th and early 19th centuries.
The town of Middlesboro, built in the crater, was established in 1886 to exploit iron and coal deposits, although the town's founder, Alexander A. Arthur, apparently did not know of the crater's extraterrestrial origin. K. J. Englund and J. B. Roen, working for the U. S. Geological Survey, identified the impact basin in 1962.
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 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.
Without Middlesboro crater, it would have been difficult for packhorses to navigate this gap, formed by differential erosion along one of the subsequent cross faults, 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).
While coal mining is still the town's primary economic driver, local leaders hope to turn the crater into a tourist destination. In 2003, the Kentucky Society of Professional Geologists designated the area a Distinguished Geologic Site, and the construction of the Cumberland Gap Tunnel makes the town a convenient source of supplies for visitors to Cumberland Gap National Historical Park.
- "Barringer". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2013-08-26.
- "Middlesboro". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2008-12-30.
-  Archived May 11, 2006, at the Wayback Machine
- K. A. Milam, J. Evenick, and B. Deane eds. "Field Guide to the Middlesboro and Flynn Creek Impact Structures" (PDF). Impact Field Studies Group. Archived from the original (PDF) on January 6, 2014. Retrieved November 13, 2012.CS1 maint: multiple names: authors list (link) CS1 maint: extra text: authors list (link)
- Kortenkamp, Steve (Summer 2004). "Impact at Cumberland Gap: Where Natural and National History Collide". PSI Newsletter. 5 (2): 1–2.
- "Kentucky town sees a future in its crater". St. Petersburg Times. Associated Press. 2003-09-20. Retrieved September 16, 2006.
- Kortenkamp, Steve (Summer 2004). "Impact at Cumberland Gap: Where Natural and National History Collide" (PDF). PSI Newsletter. 5 (2): 1–2.