The waterfall is formed by the erosion of limestone strata by the Muga River.
The name 'La Caula' is locally associated with the historical irrigation and hydraulic structures that once operated in the area.
The surrounding rock strata contain fossilized marine evidence dating back to the Eocene epoch.
The site serves as a natural transition point between the Empordà plain and the mountainous terrain of the Salines range.
Salt de La Caula is a waterfall located in the Alt Empordà region of Girona, situated along the Muga River. The waterfall features a vertical drop of approximately 30 meters over a limestone cliff face. It is positioned near the village of Boadella i les Escaules. The site is a popular destination for local hiking, as it features a series of natural pools and rock formations. The water flow is highly dependent on recent rainfall, often reducing to a trickle during dry summer months. The surrounding terrain is characterized by Mediterranean vegetation and geological formations typical of the Pre-Pyrenees foothills.
The lower observation point located at the base of the main waterfall cliff.
Wear sturdy footwear with good grip as the paths around the waterfall are uneven and slippery.
Check local rainfall reports before visiting to ensure the waterfall is actively flowing.
Bring a backpack to carry out all waste, as there are no trash facilities on-site.
Do not attempt to swim in the lower pools during high-flow periods, as strong currents and hidden submerged rocks present safety risks.
Stay on marked trails to protect the fragile riparian ecosystem and prevent soil erosion.
