The waterfall is divided into two distinct cascades, with the upper section measuring 13 meters and the lower section 10 meters.
The water originates from springs located directly beneath the north face of Giewont.
The name 'Siklawica' is derived from the term 'sikla', which is local dialect for a steep, rocky mountain stream.
The base of the waterfall is accessible via a short, stone-paved path that deviates from the main valley trail.
The site experiences significant variation in water volume, occasionally drying up during sustained periods of summer drought.
Wodospad Siklawica is a 23-meter high, two-tiered waterfall located within the Tatra National Park in Poland. It is fed by the Strążyski Stream, which originates from the northern slopes of Giewont mountain. The waterfall drops into a distinct, shallow rocky pool surrounded by a dense spruce forest. It is situated at the terminus of the Strążyska Valley trail. The water flow is most prominent during spring snowmelt and following heavy rainfall. The site serves as a frequent turnaround point for hikers traversing the valley floor. Geologically, it is formed by limestone and dolomite rocks characteristic of the Western Tatra range.
The small wooden footbridge positioned directly facing the lower cascade.
Wear footwear with high-traction soles as the rocks surrounding the pool are consistently wet and slippery.
Bring a waterproof jacket if visiting shortly after rain, as the mist at the base can be heavy.
Use the trail early in the morning to avoid high concentrations of hikers in the narrow valley path.
Do not attempt to climb the wet rocks adjacent to the falls, as they are prone to rockfall and are extremely slippery.
The trail is accessible year-round, but deep winter snow may require specialized equipment like micro-spikes.
Stay on marked trails to protect the surrounding National Park ecosystem; do not bathe in the pool.
