Cumberland Gap National Historical Park

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Cumberland Gap National Historical Park Creating a Legacy: Cumberland Gap National Historical Park July 4, 2009 marked the 50th anniversary of the dedication of Cumberland Gap National Historical Park, located at the junction of Tennessee, Virginia and Kentucky. The idea of creating a park around Cumberland Gap was talked about as early as the 1920s by the Middlesboro Kiwanis Club. Motives behind the creation of the park included saving the mountains from the continued effects of coal mining and providing additional revenue for the area. Although the creation of the park was authorized in 1940, the visitor center in Middlesboro did not open until 1955 due to World War II. When the park was officially dedicated on July 4, 1959, Vice President Richard Nixon, Secretary of the Interior Fred Seaton and Director of the National Park Service Conrad L. Wirth were among the dignitaries at the dedication. While the establishment of a national park in their community excited the residents of Middlesboro, families who lived in the rural areas of the three states felt it forever changed their traditional ways of life. Recollections of people who used to call the park lands their home sharply contrast with the stories of those who were passionate about the park’s creation. Oral history interviews with former residents and people involved with the creation of the park can be found at http://passtheword.ky.gov. (Photo courtesy of Cumberland Gap National Historical Park) Pass the Word” is a discovery tool for oral histories throughout the state of Kentucky. To learn more about this topic, visit http://passtheword.ky.gov. .
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  • Topography Along the Virginia-Kentucky Border
    Preface: Topography along the Virginia-Kentucky border. It took a long time for the Appalachian Mountain range to attain its present appearance, but no one was counting. Outcrops found at the base of Pine Mountain are Devonian rock, dating back 400 million years. But the rocks picked off the ground around Lexington, Kentucky, are even older; this limestone is from the Cambrian period, about 600 million years old. It is the same type and age rock found near the bottom of the Grand Canyon in Colorado. Of course, a mountain range is not created in a year or two. It took them about 400 years to obtain their character, and the Appalachian range has a lot of character. Geologists tell us this range extends from Alabama into Canada, and separates the plains of the eastern seaboard from the low-lying valleys of the Ohio and Mississippi rivers. Some subdivide the Appalachians into the Piedmont Province, the Blue Ridge, the Valley and Ridge area, and the Appalachian plateau. We also learn that during the Paleozoic era, the site of this mountain range was nothing more than a shallow sea; but during this time, as sediments built up, and the bottom of the sea sank. The hinge line between the area sinking, and the area being uplifted seems to have shifted gradually westward. At the end of the Paleozoric era, the earth movement are said to have reversed, at which time the horizontal layers of the rock were uplifted and folded, and for the next 200 million years the land was eroded, which provided material to cover the surrounding areas, including the coastal plain.
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  • Cumberland Gap National Historical Park Foundation Document Overview
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  • Cumberland Gap National Park
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  • Cumberland Gap U.S
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