The waterfall is classified as a 'waterfall of the tectonic type' because it forms over a displacement of rock strata.
The sandstone ledge forming the drop is significantly more resistant to erosion than the underlying rock layers, which keeps the waterfall feature stable over time.
It is the highest waterfall located within the entire Beskid mountain range.
The site was officially declared a protected natural monument in 1991.
The waterfall is located at an altitude of approximately 600 meters above sea level.
Wodospad w Sopotni Wielkiej is the largest waterfall in the Beskid Żywiecki mountain range, standing at 12 meters in height. It is situated on the Sopotnianka stream and represents a rare geological formation in the Flysch Carpathians. The waterfall is designated as a nature monument due to its unique geological structure, consisting of a distinct tectonic fault. The stream flows over a resistant sandstone ledge, creating a vertical drop that is visually prominent. The site is part of the Żywiec Landscape Park, protecting the surrounding forest and river ecosystem. Public access is provided via a small viewing platform and a path leading to the base of the cascade. The area is relatively accessible, requiring a short walk from the village road.
The wooden bridge and viewing platform directly facing the base of the waterfall.
Wear footwear with good grip as the rocks surrounding the waterfall pool can be extremely slippery.
Visit immediately after heavy rainfall to see the waterfall at its most powerful volume.
Parking is limited in the village, so plan for a short walk from available roadside spots.
Attempting to climb the steep, wet rock faces around the waterfall, which are dangerous.
Respect the nature reserve status by staying on marked paths and carrying out all litter.
