Greenbrier River Trail

The Greenbrier River Trail is a 78-mile rail-trail following the former Greenbrier Division of the Chesapeake and Ohio Railway along the Greenbrier River from Cass in Pocahontas County to Caldwell near Lewisburg in Greenbrier County. Designated as a state park in 1980, it is the longest trail of its kind in West Virginia and one of the oldest rail-trails in the United States. The trail passes through scenic mountain landscapes, connecting communities including Marlinton, and skirting Seneca State Forest, Watoga State Park, and Calvin Price State Forest. Features include 37 original railroad bridges and two tunnels dating from the turn of the twentieth century. A Rails to Trails Conservancy Hall of Famer and one of 52 Millennium Legacy Trails, the Greenbrier River Trail was added to the National Trails System in June 2021, recognizing its outstanding recreational and historical value.

The Greenbrier River Trail corridor supports diverse wildlife communities along its 78-mile length through the mountain valleys of southeastern West Virginia. The Greenbrier River itself harbors smallmouth bass, rock bass, channel catfish, and native brook trout in its cooler tributary streams. White-tailed deer are abundant along the trail, frequently observed during early morning and evening hours. Black bear, wild turkey, and ruffed grouse inhabit the forested hillsides flanking the trail. The river corridor serves as an important habitat for great blue herons, belted kingfishers, and various waterfowl species. Songbird diversity is high during the breeding season, with warblers, vireos, and thrushes nesting in the riparian forests. River otters have been reintroduced to the Greenbrier River system and are occasionally spotted by trail users. The trail's linear nature provides an important wildlife corridor connecting habitats across multiple state forests and parks.

The vegetation along the Greenbrier River Trail transitions through several forest communities reflecting the varied terrain and elevation changes along its 78-mile course. Riparian zones along the river feature sycamore, river birch, box elder, and various willow species adapted to periodic flooding. The lower slopes support rich mixed mesophytic forest with tulip poplar, sugar maple, basswood, and white ash. Higher elevations along the trail's northern sections near Cass include red spruce and northern hardwood forests typical of the Allegheny Mountains. Rhododendron and mountain laurel form dense evergreen thickets along many sections of the trail, providing spectacular bloom displays in late spring and early summer. The trail corridor supports diverse wildflower communities, including jack-in-the-pulpit, cardinal flower, and various species of goldenrod and aster. Invasive plant species including Japanese knotweed and multiflora rose require ongoing management in disturbed areas along the former railroad grade.

The Greenbrier River Trail traverses a geological cross-section of the Valley and Ridge and Allegheny Plateau provinces of the central Appalachian Mountains. The trail follows the Greenbrier River, which has carved its valley through a sequence of Paleozoic sedimentary rocks spanning from the Ordovician through the Pennsylvanian periods, representing approximately 200 million years of geological history. The prominent Greenbrier Limestone, a Mississippian-age formation, underlies much of the valley and has been dissolved by groundwater to create extensive karst topography including caves and sinkholes. The two railroad tunnels along the trail, the 511-foot Sharps Tunnel built in 1899 and the 402-foot Droop Mountain Tunnel built in 1900, were cut through resistant sandstone formations. The relatively gentle gradient of the trail, originally engineered for railroad use, provides evidence of the river's geological history as it meanders through alternating narrows and broader valley sections carved through rocks of varying resistance.

The Greenbrier River Trail experiences a humid continental climate with significant variation along its 78-mile length due to changes in elevation, valley orientation, and proximity to mountain barriers. The southern terminus near Caldwell sits at approximately 1,600 feet elevation, while the northern end at Cass reaches about 2,450 feet, creating cooler conditions at the trail's upper sections. Summer temperatures typically range from the low 70s to mid-80s Fahrenheit, making the shaded river corridor a pleasant destination for warm-weather recreation. Winters are cold, with temperatures frequently dropping below freezing and snowfall accumulations ranging from 30 inches in the south to over 60 inches near Cass. Annual precipitation averages 40 to 45 inches, with spring and summer receiving slightly more rainfall. The trail surface can become muddy during wet periods, particularly in spring. Autumn brings spectacular foliage displays, with peak color typically occurring in mid-October along the trail corridor.

The Greenbrier River Valley has been inhabited for thousands of years, with archaeological evidence of Native American use dating back to the Archaic period. European settlement began in the mid-eighteenth century as pioneers moved into the fertile valley bottomlands. The region's vast timber resources attracted the railroad industry in the late nineteenth century, with the Chesapeake and Ohio Railway constructing its Greenbrier Division to haul lumber to market. The railroad transformed the valley's economy, supporting sawmills, tanneries, and small communities along its route. Notably, the Cass mill at the trail's northern terminus supplied spruce wood to the Wright Brothers for use in their early aircraft. The town of Marlinton, the largest community along the trail, developed as a railroad town and county seat. Passenger service continued until 1958, while freight operations persisted until the line was officially abandoned on December 29, 1978.

The Greenbrier River Trail's transformation from active railroad to recreational trail began shortly after the Chesapeake and Ohio Railway ceased operations. The tracks were removed in 1979, and on March 24, 1980, Governor Jay Rockefeller signed legislation creating the Greenbrier River Trail State Park. The C&O donated most of its right-of-way south of Durbin to the state on June 20, 1980. Mark Hankins of Lewisburg, whose grandfather and father had planned the Greenbrier Division as engineers, was instrumental in acquiring the right-of-way. The abandoned rail bed was converted to a multiuse trail managed by the West Virginia Division of Natural Resources. The trail has received numerous accolades, including designation as a Rails to Trails Conservancy Hall of Famer, selection as one of 52 Millennium Legacy Trails, and a top-ten hiking trail ranking by Backpacker Magazine. Its addition to the National Trails System in 2021 further cemented its status as a premier recreational resource.

The Greenbrier River Trail stretches 78 miles from Cass to Caldwell, offering a gentle, mostly flat surface suitable for hiking, biking, and horseback riding. The trail features 37 original railroad bridges crossing the Greenbrier River and its tributaries, each offering scenic views of the mountain landscape. Two historic tunnels provide unique passage through the mountains: the 511-foot Sharps Tunnel, built in 1899, and the 402-foot Droop Mountain Tunnel, completed in 1900. The trail passes through the charming town of Marlinton, which offers services and access to the Pocahontas County seat. Notable nearby attractions accessible from the trail include Watoga State Park, Seneca State Forest, Calvin Price State Forest, Droop Mountain Battlefield State Park, and the Cass Scenic Railroad. The river itself provides excellent opportunities for fishing, swimming, and paddling alongside the trail. Multiple access points allow users to complete shorter sections.

The Greenbrier River Trail is accessible from numerous trailheads along its 78-mile length, with major access points at Cass, Marlinton, Seebert, Renick, and Caldwell. Parking areas are provided at most trailheads. The trail surface consists of packed gravel and crushed limestone suitable for hiking, mountain biking, and horseback riding. Several shuttle services operate along the trail, allowing point-to-point trips. Overnight accommodations are available in Marlinton, at nearby state parks including Watoga and Seneca, and at various bed-and-breakfast establishments along the trail corridor. Primitive camping is permitted at designated sites. Bicycle rentals are available from outfitters in Marlinton and other communities. The trail is open year-round, though winter conditions may limit accessibility in some sections. The nearest commercial airports are in Lewisburg and Charleston, with Lewisburg approximately 30 miles from the southern trailhead.

The Greenbrier River Trail represents a successful model of adaptive reuse, converting abandoned railroad infrastructure into a major recreational and economic resource while preserving the natural corridor along the Greenbrier River. Trail maintenance requires ongoing management of the crushed stone surface, bridge inspections, and vegetation control along the 78-mile corridor. The trail has generated significant economic benefits for communities along its route, with businesses increasing tenfold and tourism becoming an important economic driver for the region. Environmental stewardship along the trail includes management of invasive plant species, protection of riparian buffers, and cooperation with adjacent state forests and parks on landscape-scale conservation efforts. The Greenbrier River itself faces water quality challenges from agricultural runoff and historical mining impacts, and the trail corridor provides an important buffer zone along the river. Community volunteer groups and trail organizations contribute to maintenance and improvement projects throughout the year.