The diatomite excavated here was historically used in the manufacturing of dynamite and as a polishing agent.
The cliffs surrounding the falls contain significant Jurassic fossil beds.
The waterfall is bifurcated by a large rock formation in its upper section during periods of high rainfall.
The local rock formations are part of the Trotternish Escarpment, one of the largest landslides in Britain.
The site remains one of the few places on the island where historical industrial ruins are integrated directly into a natural waterfall setting.
Lealt Falls is located on the Trotternish Peninsula on the Isle of Skye, featuring a waterfall that plunges 90 meters into a deep gorge before meeting the sea. The site sits at the edge of a dramatic sea cliff formed by layers of Jurassic shale and sandstone. A series of concrete ruins remain from a 19th-century diatomite processing plant that once operated at the mouth of the river. The waterfall originates from the Lealt River, which flows from Loch Corcasail. Visitors can access a viewing platform that overlooks both the falls and the coastal cliffs. The area is defined by its exposed geological strata and rugged Atlantic outlook. The site is a frequent stop on the A855 road circuit around the island's northeast coast.
The fenced viewing platform provides the optimal angle for capturing both the vertical drop of the falls and the coastal horizon.
Walk the gravel path beyond the initial viewing platform to see the ruins of the old diatomite factory.
Bring windproof layers, as the cliff-side exposure makes the area significantly colder than inland locations.
Stay on marked paths, as the steep cliffs and loose shale near the gorge edges are unstable.
Do not attempt to climb down into the gorge, as the terrain is prone to rockfalls and slippery surfaces.
Wear sturdy, waterproof hiking boots with good grip; keep dogs on a leash due to steep, unguarded drops.
