The Foothills Parkway is a national parkway which, if completed, will traverse the foothills of the northern Great Smoky Mountains in East Tennessee, located in the Southeastern United States. The 71-mile (114 km) parkway will ideally connect U.S. Route 129 along the Little Tennessee River in the west with Interstate 40 along the Pigeon River in the east, passing through parts of Blount County, Sevier County, and Cocke County. Large sections of the parkway will cross a series of high ridges running roughly parallel to the Tennessee boundary of the Great Smoky Mountains National Park, and will offer unobstructed views of the Great Smokies to the south and the Tennessee Valley to the north.
The oldest unfinished highway project in Tennessee, the Foothills Parkway project has been continuously stalled by funding difficulties since Congress authorized its construction in 1944. As of 2007, only 1/3 of the parkway had been completed and opened to vehicular traffic. The longest open section consists of a leg traversing the western flank of Chilhowee Mountain in Blount County, connecting US-129 along the Chilhowee Lake impoundment of the Little Tennessee River with U.S. Route 321 in the town of Walland. The other open section is a stretch traversing Green Mountain in Cocke County, connecting US-321 in Cosby with Interstate 40 in the Pigeon River valley. The Gatlinburg Bypass, which traverses the eastern flank of Cove Mountain between Pigeon Forge and the national park, is also considered part of the parkway.
The parkway is currently managed by the National Park Service.
The Foothills of the Great Smokies consist of a series of low mountains and hills lying roughly between the Great Smoky Mountains National Park to the south and the flatlands of the Tennessee River and French Broad River valleys to the north. The most prominent of the Foothills are characterized by long-but-narrow ridges, running parallel to the crest of the Smokies, similar to a circuit wall surrounding a medieval castle.
Although the average elevation of the Foothills is relatively low, a high topographic prominence is not uncommon among these ridges, due to their detachment from the main crest of the Smokies. English Mountain (3,629 ft), one of the highest of the Foothills, is the fifth most prominent mountain in Tennessee, and dominates the view south of Interstate 40 for a considerable stretch between Sevierville and Newport. Chilhowee Mountain, located mostly in Blount County, is the first major geological structure visible when approaching the mountains via Lamar Alexander Parkway (US-321), and its eastern flank, known as "The Three Sisters," is visible from almost anywhere in Maryville.
Geologically, the Foothills largely consist of Cambrian Class III rocks of the Paleozoic period, a type known specifically as the Chilhowee Group. Chilhowee Group rocks, which are mostly sandstones, siltstones, and shales, range in age from about 300 million to 500 million years old. Thus, the rocks of the Foothills are much younger than the billion-year old Precambrian Ocoee Supergroup rocks that form the crest and higher ridges of the Great Smokies range.
The most prominent of the Foothills include:
Chilhowee Mountain — a narrow ridge stretching between the Little Tennessee River (specifically the river's Chilhowee Lake impoundment) and the Little Pigeon River valley to the east. While the mountain is long, it rarely reaches a width of more than 3 or . Little River cuts a large gap in the middle of the mountain (near Walland), dividing it into eastern and western sections. The highest point on eastern section is 2,843 feet (866m) and the highest point on the western section is 2,650 feet (807m) at a knob known as Look Rock.
Bates Mountain — a low, bulky ridge between Miller Cove and Tuckaleechee Cove. Bates' highest point is just over . Although Bates lacks the dramatic "backbone" formation of Chilhowee, a rocky gorge on its south flank cut by Carr Creek has presented numerous construction challenges for the parkway project.
Cove Mountain — a large ridge situated between Wears Valley to the west, Gatlinburg to the east, and Pigeon Forge to the north. The national park boundary traverses part of the crest of Cove Mountain. The mountain's elevation reaches 4,077 feet (1,243m) at its summit.
Webb Mountain — a long, narrow ridge stretching roughly from the Middle Prong of the Little Pigeon River in the west to the Cosby area in the east, a distance of roughly 10 miles (14 km). Webb Mountain dominates the view north of US-321 between Pittman Center and Cosby. Its summit, near the middle of the ridge, is 3,100 feet (945m) above sea level.
Green Mountain — a small mountain stretching between Cosby to the west and the Pigeon River valley to the east. Its highest point is 2,785 feet (849m) above sea level.
English Mountain, the highest of the Foothills at 3,629 feet (1,112m), stretches for nearly between the East Fork of the Little Pigeon and Newport, paralleling the shores of Douglas Lake. Hall Top (Stone Mountain) rises prominently opposite Green Mountain above the Pigeon River valley. The parkway will not cross any part of English Mountain or Hall Top, however.
The Foothills of the Great Smokies were drawing tourists as early as the mid-1800s. Most visitors during this period came for the area's mineral-rich mountain springs, which were thought to have health-restoring qualities. Resort hotels quickly sprang up throughout the Foothills, becoming popular summer-time destinations for Knoxville's upper class. The most successful of these resorts were Montvale Springs and Alleghany Springs at the base of Chilhowee Mountain, Kinzel Springs in Tuckaleechee, Line Springs in Wears Valley, and Carson Springs near Newport.
Just before the Civil War, author Sidney Lanier spent several summers at Montvale Springs. The Chilhowee Mountain area would be a major influence on the setting for his first novel, Tiger Lilies. In 1885, Mary Noailles Murfree, one of the first authors to popularize the natural wonders of the Smokies, wrote:
"... Chilhowee Mountain, rising up, massive and splendid, against the west. The shadows of the clouds flecked the pure and perfect blue of the sunny slopes with a dusky motling of purple.
The original plan for the Great Smoky Mountains National Park included much of the Foothills within the proposed park boundaries, although by the time the park opened in 1934, the boundary had been moved south of Townsend and Wears Valley.
When Congress authorized the construction of the Blue Ridge Parkway in the 1930s, it was decided that no part of the parkway would pass through Tennessee (the goal of the parkway was to connect the Great Smoky Mountains National Park with Shenandoah National Park). Disappointed, Frank Maloney, who was vice-president of the Great Smoky Mountains Conservation Association, began lobbying for a parkway to connect the recreational areas on the Tennessee side of the Great Smokies.
In 1944, after extensive lobbying by Congressman B. Carroll Reece, Congress authorized construction of a road connecting US-129 at Chilhowee Lake and I-40 along the Pigeon River. In 1945, the Tennessee state legislature authorized the Tennessee Highway Department to buy rights-of-way for the road, and a second bill in 1947 authorized the transfer of rights-of-way to the National Park Service.
While the early bureacratic hurdles had been cleared, the Tennessee Highway Department moved slowly in purchasing the road's rights-of-way. In 1956, park superintendent Edward Hummel managed to get the Foothills Parkway project included in the National Park Service's Mission 66 program, assuring early construction funds. Shortly thereafter, Governor Frank G. Clement authorized the THD to begin buying rights-of-way. Construction finally began in 1960.
The original plan for Foothills Parkway called for eight sections:
After the initial progress in the 1960s, the project again stalled in the 1970s due to funding cuts. By 1978, less than one-third of the proposed parkway had been completed. Construction on the two sections between Walland and Wears Valley finally began in 1984, but after some progress, was halted due to erosion and environmental issues, specifically the spilling of sulfuric acid into nearby streams. The corridor's route was redesigned, and construction began again in 1994. Tennessee Congressmen John Duncan, Jr. and James Quillen have been instrumental in obtaining federal funding for the project since the 1980s.
In recent years, the Foothills Parkway project has become controversial due to the already-high volume of vehicular traffic that passes through the Smokies each year. Some argue that the parkway will add to the congestion, while others say it will help relieve congestion by drawing off some of the park's traffic. Furthermore, because parkways always seem to rank low in budgetary priorities, it will likely take several decades to complete the entire parkway. The major influence for Foothills Parkway— the Blue Ridge Parkway— took several decades to complete; likewise, construction on the Natchez Trace Parkway— which began in 1939— was not completed until 2005.
Construction on Foothills Parkway has continued into the 21st century, although progress has been slow. A particularly difficult section of the Walland-Wears Valley corridor, now known as the "Missing Link," will require a series of 10 bridges over a section straddling the Sevier County-Blount County line. Two of these were completed in 2001. In late May 2005, the Federal Highway Administration awarded a contract to build Bridge Number 8, the third of these bridges. This new bridge will be 220 feet (67 m) in length, and is slated for completion in late 2007. When the other seven bridges are eventually constructed, the "missing link" will open up a stretch of road 16.1 miles (25.9 km) long.
Although no funding has been set aside for the remaining sections of the parkway between Wears Valley and Cosby, the government still owns the rights-of-way, and their completion has not been ruled out. In early 2007, the National Park Service began conducting an environmental impact assessment and collecting public input regarding Section 8B (Pittman Center to Cosby).
Much like the Blue Ridge Parkway, Foothills Parkway traverses what would be otherwise-roadless ridge crests, allowing for spectacular views of the surrounding areas.
The Chilhowee section of the parkway, which has been open since 1966, has 8 overlooks on its south side, looking into the Smokies, and 4 overlooks on its north side, looking into the Tennessee Valley. An observation tower has been placed atop Look Rock, allowing for a 360-degree view of the Western Smokies and Blount County. A half-mile trail connects the tower to a parking area along the parkway.
Several of the highest mountains in the Smokies can be seen from Look Rock. Clingmans Dome and Thunderhead Mountain are visible to the south, and Mount Le Conte is visible to the southeast. On a clear day, the high peaks of the Eastern Smokies— Mount Guyot, Mount Chapman, and Old Black— are visible toward the east. The Rich Mountain/Cades Cove Mountain massif dominates the view immediately to the south and southeast. Gregory Bald rises like a giant dome to the southwest. To the west, the Yellow Creek section of the Unicoi Mountains is visible, along with a dramatic view of Chilhowee's crest.
Looking north from Look Rock, most of Blount County and parts of Loudon County and Monroe County are visible. McGhee-Tyson Airport presents as a long greenish strip to the north, and the lights of South Knoxville begin to appear around sunset. The Cumberland Plateau dominates much of the northern horizon.
Foothills Parkway crosses Green Mountain in diagonal fashion, traversing the southwest and northeastern flanks of the mountain. From the southwest section, Mount Cammerer and the Eastern Smokies dominate the view. From the northeast section, English Mountain presents as a large ridge to the northwest, and Hall Top rises in peak-like fashion to the east. The lights of Newport are visible early in the morning and later in the evening.