See C. C. Campbell, Birth of a National Park in the Great Smoky Mountains (1978); M. Frome, Strangers in High Places: The Story of the Great Smoky Mountains (1980).
West range of the Appalachian Mountains in the U.S. It extends along the North Carolina–Tennessee boundary and blends into the Blue Ridge to the east. The highest part lies within the Great Smoky Mountains National Park and includes Clingmans Dome, which at 6,643 ft (2,025 m) is the highest peak. Covered by forests, it was originally the domain of the Cherokee, and the area includes the Cherokee Indian Reservation and parts of the Pisgah and Cherokee national forests. The mountains form a popular resort area that includes part of the Appalachian National Scenic Trail and the Blue Ridge Parkway.
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Great Smoky Mountains National Park is a United States National Park that straddles the ridgeline of the Great Smoky Mountains, part of the Blue Ridge Mountains which are a division of the larger Appalachian Mountain chain. The border between Tennessee and North Carolina runs northeast to southwest through the centerline of the park. It is the most visited national park in the United States. On its route from Maine to Georgia, the Appalachian Trail also passes through the center of the park. The park was chartered by the United States Congress in 1934 and officially dedicated by President Franklin Delano Roosevelt in 1940 . It encompasses 814 square miles (2,108 km²), making it one of the largest protected areas in the eastern United States. The main park entrances are located along U.S. Highway 441 (Newfound Gap Road) at the towns of Gatlinburg, Tennessee, and Cherokee, North Carolina.
As white settlers moved in, logging grew as a major industry in the mountains, and a rail line, the Little River Railroad, was constructed in the late 19th century to haul timber out of the remote regions of the area. Cut-and-run style clearcutting was destroying the natural beauty of the area, so visitors and locals banded together to raise money for preservation of the land. The U.S. National Park Service wanted a park in the eastern United States, but did not want to spend much money to establish one. Though Congress had authorized the park in 1926, there was no nucleus of federally-owned land around which to build a park. John D. Rockefeller, Jr. contributed $5 million, the U.S. government added $2 million, and private citizens from Tennessee and North Carolina pitched in to assemble the land for the park, piece by piece. Travel writer Horace Kephart and photographer George Masa were instrumental in fostering the development of the park. The park was officially established on June 15, 1934. During the Great Depression, the Civilian Conservation Corps, the Works Progress Administration, and other federal organizations made trails, fire watchtowers, and other infrastructure improvements to the park and Smoky Mountains.
The wide range of elevations mimics the latitudinal changes found throughout the entire eastern United States. Indeed, ascending the mountains is comparable to a trip from Tennessee to Canada. Plants and animals common in the country's Northeast have found suitable ecological niches in the park's higher elevations, while southern species find homes in the balmier lower reaches.
During the most recent ice age, the northeast-to-southwest orientation of the Appalachian mountains allowed species to migrate southward along the slopes rather than finding the mountains to be a barrier. As climate warms, many northern species are now retreating upward along the slopes and withdrawing northward, while southern species are expanding.
The park normally has very high humidity and precipitation, averaging from 55 inches (1,400 mm) per year in the valleys to 85 inches (2,200 mm) per year on the peaks. This is more annual rainfall than anywhere in the United States outside the Pacific Northwest and parts of Alaska. It is also generally cooler than the lower elevations below, and most of the park has a humid continental climate more comparable to locations much farther north, as opposed to the humid subtropical climate in the lowlands. The park is almost 95 percent forested, of which roughly a quarter is old growth with many trees that predate European settlement of the area. It is one of the largest blocks of deciduous, temperate, old growth forest in North America.
The variety of elevations, the abundant rainfall, and the presence of old growth forests give the park an unusual richness of biota. About 10,000 species of plants and animals are known to live in the park, and estimates as high as an additional 90,000 undocumented species may also be present.
Park officials count more than 200 species of birds, 66 species of mammals, 50 species of fish, 39 species of reptiles, and 43 species of amphibians, including many lungless salamanders. The park has a noteworthy black bear population, numbering at least 1,800. An experimental re-introduction of elk (wapiti) into the park began in 2001.
Over 100 species of trees grow in the park. The lower region forests are dominated by deciduous leafy trees. At higher altitudes, deciduous forests give way to coniferous trees like Fraser Fir. In addition, the park has over 1,400 flowering plant species and over 4,000 species of non-flowering plants.
The Great Smoky Mountains National Park is a major tourist attraction in the region; over 9 million tourists and 11 million non-recreational visitors traveled to the park were recorded in 2003, double that of any other national park. Surrounding towns, notably Gatlinburg, Pigeon Forge, Sevierville, and Townsend, Tennessee, and Cherokee, Sylva, Maggie Valley, and Bryson City, North Carolina receive a significant portion of their income from tourism associated with the park.
The two main visitors' centers inside the park are Sugarlands Visitors' Center near the Gatlinburg entrance to the park and Oconaluftee Visitors' Center near Cherokee, North Carolina at the eastern entrance to the park. These ranger stations provide exhibits on wildlife, geology, and the history of the park. They also sell books, maps, and souvenirs.
U.S. Highway 441 (known in the park as Newfound Gap Road) bisects the park, providing automobile access to many trailheads and overlooks, most notably that of Newfound Gap. At an elevation of 5,048 feet (1,539 m), it is the lowest gap in the mountains and is situated near the center of the park, on the Tennessee/North Carolina state line, halfway between the border towns of Gatlinburg and Cherokee. It was here that in 1940, from the Rockefeller Memorial, Franklin Delano Roosevelt dedicated the national park. On clear days Newfound Gap offers arguably the most spectacular scenes accessible via highway in the park.
The park has a number of historical attractions. The most well-preserved of these (and most popular) is Cades Cove, a valley with a number of preserved historic buildings including log cabins, barns, and churches. Cades Cove is the single most frequented destination in the national park. Self-guided automobile and bicycle tours offer the many sightseers a glimpse into the way of life of old-time southern Appalachia. Other historical areas within the park include Roaring Fork, Cataloochee, Elkmont, and the Mountain Farm Museum and Mingus Mill at Oconaluftee.
There are 850 miles (1,368 km) of trails and unpaved roads in the park for hiking, including seventy miles of the Appalachian Trail. . Mount Le Conte is one of the most frequented destinations in the park. Its elevation is 6,593 feet (2,010 m) — the third highest summit in the park and, measured from its base to its highest peak, the tallest mountain east of the Mississippi River. Its Alum Cave Trail, which is the most heavily used of the five paths en route to the summit, provides many scenic overlooks and unique natural attractions such as Alum Cave Bluffs and Arch Rock. Hikers may spend a night at the LeConte Lodge, located near the summit, which provides cabins and rooms for rent (except during the winter season). Accessible solely by trail, it is the only private lodging available inside the park.
Another popular hiking trail leads to the pinnacle of the Chimney Tops, so named because of its unique dual-humped peaktops. This short but strenuous trek rewards nature enthusiasts with a spectacular panorama of the surrounding mountain peaks.
Both the Laurel Falls and Clingman's Dome trails offer relatively easy, short, paved paths to their respective destinations. The Laurel Falls Trail leads to a powerful 80 foot (24 m) waterfall, and the Clingman's Dome Trail takes visitors on an uphill climb to a fifty-foot observation deck, which on a clear day offers views for many miles over both the Tennessee and North Carolina mountains.
In addition to day hiking, the national park offers opportunities for backpacking and camping, particularly via the placement of shelters along the Appalachian Trail; designated campsites are also scattered throughout the park. Permits are required for stays at both locales and are almost always valid for only one night.