The waterfall is formed by the Rupit stream cutting through layers of volcanic basalt and sandstone.
The cliff face at Salt de Sallent is part of the Collsacabra mountain range, known for its significant seismic history.
The stream flow is seasonal, often appearing as a trickle during dry summer months.
The waterfall is situated along a tectonic fault line that helped shape the precipitous drop-off.
The area is home to diverse bird species including peregrine falcons that nest in the rocky outcrops.
Salt de Sallent is a 115-meter vertical waterfall located on the edge of a sheer cliff near the medieval village of Rupit. It serves as the primary drainage point for the Rupit stream before it flows into the Susqueda Reservoir. The hiking trail leading to the waterfall originates in Rupit and traverses through basaltic rock formations and oak forests. The site is a geological landmark shaped by intense volcanic activity in the Collsacabra region. Visitors can view the falls from a clifftop vantage point or descend into the canyon for a bottom-up perspective. The flow rate is highly dependent on recent rainfall and can fluctuate significantly between seasons.
The designated cliff-edge viewing platform located at the top of the waterfall trail.
Wear sturdy hiking boots with aggressive tread for the steep, uneven descent into the valley.
Bring a waterproof jacket if visiting after a heavy rainfall to manage the high volume of mist and spray.
Carry a portable power bank, as cell reception can be spotty within the deeper sections of the canyon.
Attempting the hike in high-top street shoes or flip-flops; ignoring weather forecasts, as the trail becomes slippery and dangerous after rain.
Practice 'leave no trace' principles by packing out all trash; maintain a safe distance from cliff edges as there are no perimeter fences.
