Moonshiner 28

Deals Gap to Highlands

Western North Carolina · North Carolina · United States

Key measurements

Distance

74.5 miles

Elevation gain

9,632 ft

Elevation loss

7,492 ft

High point

3,844 ft

Low point

1,286 ft

Net change

2,140 ft (1,693 ft to 3,833 ft)

Surface

Paved

Route type

point-to-point

Route Overview

Moonshiner 28 follows North Carolina Highway 28 for 74.6 miles from Deals Gap to Highlands, cutting through the Southern Blue Ridge along Fontana Lake, the Little Tennessee River, Franklin, and the Cullasaja Gorge. Beginning near the US-129 junction outside Robbinsville, the route drops into the Cheoah River corridor before winding along the steep timbered shoreline of Fontana Lake. From there, it passes through the quieter agricultural pockets of the Stecoah Valley, continues south into the Little Tennessee River basin toward Franklin, and finishes with a steep climb through the Cullasaja River Gorge onto the Highlands Plateau.

Key Segments & Geographic Transitions

Fontana Rim to Little Tennessee Basin — Miles 0.0–57.3

Starting near the Cheoah Dam area, NC-28 hugs the northern contours of Graham and Swain counties. The road works through continuous technical curves along the ridge above Fontana Lake before easing into the open floor of Stecoah Valley. As it crosses US-19 near Almond, the road heads due south, following the Little Tennessee River south through Macon County. The topography along this stretch offers wide, sweeping turns through mountain farm country, bordered by the Cowee and Nantahala mountain ranges.

Franklin Confluence Corridor — Miles 57.7–61.6

Approaching Franklin, NC-28 briefly merges with US-64 East. This short transitional corridor carries you around the edge of Franklin’s valley basin, bridging the lower agricultural terrain with the canyon approach ahead. Traffic density increases here as regional routes converge before heading into the mountains.

Cullasaja Gorge Climb to Highlands — Miles 62.3–74.6

Leaving the Franklin basin behind, NC-28 runs concurrently with US-64 along the floor of the Cullasaja River Gorge. The road narrows dramatically, carved directly into vertical granite canyon walls with the river dropping away on one side and wet cliff faces overhang on the other. Tight twisties and sweeping S-bends track the river’s ascent. As the canyon tops out, the road delivers you directly onto the high plateau of Highlands, topping out at 3,844 feet above sea level.

Seasonal & Environmental Context

Elevation plays a massive role on this route. While the lower sections along Fontana Lake and Franklin sit around 1,300 to 2,000 feet, Highlands sits near 4,000 feet.

Spring & Summer: Dense forest canopy keeps lower gorge sections shaded and damp long after rainstorms pass. Summer afternoon thunderstorms roll in quickly over the crest of the Blue Ridge, bringing torrential downpours and runoff. * Autumn: Leaf season brings extraordinary color to the hardwoods, but with it comes heavy tourist traffic and leaf litter on wet asphalt. * Winter: Cold microclimates dominate the shaded rock cuts of the Cullasaja Gorge. Black ice can linger late into the morning on canyon curves and high-elevation bridges even when the valley in Franklin is dry and clear.

Logistics & Services

Fuel: Available near the starting point in the Deal's Gap/Robbinsville corridor, mid-route around Almond and Franklin, and at the end of the route in Highlands. The 50-mile stretch between Stecoah and Franklin has sparse retail, so plan fuel stops accordingly. * Cellular Coverage: Signal is weak to nonexistent through the Fontana Lake curves and inside the deep rock walls of the Cullasaja Gorge. Reliable connectivity returns near Franklin and inside Highlands town limits.

Important Considerations

Narrow Lanes & Sightlines: The Cullasaja Gorge segment (Miles 62.3–74.6) features rock overhangs, zero shoulder space, and tight blind curves. Commercial trucks and large RVs occasionally use this corridor, sometimes crossing the centerline on tight bends. * Debris & Washouts: Wet weather frequently washes gravel, small rocks, and mountain runoff across the road surface in the canyon sections.