The 'Sinks' was created by a massive log jam during the timber harvesting era, which forced the river to carve a new path through the rock.
The pool beneath the falls is significantly deeper than it appears, with underwater rock formations creating powerful recirculating currents.
The name refers to the historical observation that the water appears to 'sink' into the deep, dark pool before continuing downstream.
The geological formation is part of the Precambrian Ocoee Supergroup, composed of metasandstone and slate.
The Sinks is a high-volume waterfall on the Little River within Great Smoky Mountains National Park, characterized by a sharp bend in the watercourse that creates a deep, turbulent pool. The waterfall is formed by a geological constriction where the entire volume of the Little River is forced through a narrow gap. It is uniquely accessible, located immediately adjacent to a roadside parking area on Little River Road. The site features a rock ledge overlooking the rushing water and the deep green pool below. Historically, the area was the site of a logging splash dam operation in the early 20th century. Warning signs remain posted due to the dangerous undercurrents and hidden debris within the pool. It serves as a popular stop for motorists traveling between Gatlinburg and Townsend.
The fenced overlook platform provides a clear, safe vantage point directly above the waterfall.
Use the paved parking area directly off the road; do not attempt to park on the road shoulders.
Stay on the designated observation area to avoid the slippery, unstable rocks near the water's edge.
Bring a polarizing filter if photographing the water to reduce glare on the deep pool surface.
Do not attempt to climb down into the gorge or swim in the pool, as the area is notorious for fatal accidents and rescues.
Little River Road may experience temporary closures during winter snow or ice events.
Swimming and diving are strictly prohibited due to hazardous currents and frequent submerged debris.
