Šútovský Waterfall
Žilina Region
Šútovský Waterfall is a striking natural feature located in the Malá Fatra mountains of Slovakia, approximately 4 kilometers north of the village of Šútovo. At an elevation of 830 meters, it is the tallest waterfall in the region, boasting a height of 38 meters. The waterfall is fed by the Šútovský stream, which originates from the Mojžišove pramene rock formation about one kilometer upstream. The stream maintains a width of around 2.5 meters above the waterfall, contributing to its steady flow. Geologically, the waterfall is situated on the boundary between granites and granodiorites, with the base composed of autometamorphosed granodiorites. The waterfall's formation is linked to the uplift of the mountain range and the subsidence of the Turčianska basin. Access to the site is available via marked hiking trails from the village of Šútovo or from the Chata pod Chlebom mountain hut, making it a popular destination for nature lovers and hikers exploring the Šútovská dolina National Nature Reserve. Its impressive height, geological significance, and picturesque setting make Šútovský Waterfall a unique and inspiring natural landmark in Slovakia.
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Astuce: The best time to visit Šútovský Waterfall is during late spring to early autumn when hiking trails are most accessible and the water flow is vibrant. Visitors are advised to wear sturdy hiking shoes and follow the blue tourist trail from Šútovo village or from Chata pod Chlebom via Kopiská junction. Purchasing tickets is not required as the waterfall is in a natural reserve, but visitors should respect local conservation rules. Early morning visits can offer quieter experiences and better photo opportunities. No specific discounts apply as it is a natural site accessible freely.
Faits intéressants
- •Šútovský Waterfall is the tallest waterfall in the Malá Fatra mountains at 38 meters high.
- •The waterfall is fed by the Šútovský stream, which originates from the Mojžišove pramene rock formation about 1 kilometer upstream.
- •The geological base of the waterfall consists of autometamorphosed granodiorites, marking a boundary between granite and granodiorite formations.
- •The stream above the waterfall is approximately 2.5 meters wide, maintaining a steady flow.
- •The waterfall lies within the Šútovská dolina National Nature Reserve, a protected natural area.
Histoire
Šútovský Waterfall was formed as a result of the geological uplift of the Malá Fatra mountain range and the simultaneous subsidence of the Turčianska basin.
Its geological setting marks the boundary between granitic and granodioritic rock formations, which influenced its current structure.
The waterfall has long been recognized as the highest in the Malá Fatra region, serving as a natural landmark within the Šútovská dolina National Nature Reserve.
Over time, it has become a popular destination for hikers and nature enthusiasts exploring the region's natural heritage.
Guide du lieu
Šútovský Waterfall
The main natural attraction, a 38-meter-high waterfall fed by the Šútovský stream originating from Mojžišove pramene. It is renowned for its impressive height and geological setting within the Malá Fatra mountains.
Contact
Téléphone: 0948 938 393