The waterfall is created by travertine deposition, a geological process where lime-rich spring water precipitates minerals onto mosses and vegetation.
The 'veil' appearance is technically a series of tufa dams that have accumulated over centuries.
The water feeding the falls originates from the high-yield Szalajka Spring located further up the valley.
Geologically, the feature is a prime example of a rheocrene spring environment within the Bükk region.
Fátyol-vízesés, or Veil Waterfall, is a terraced limestone tufa formation located in the Szalajka Valley of the Bükk Mountains. The waterfall earns its name from the delicate, lace-like appearance created by water trickling over seventeen distinct limestone steps. It is a natural travertine cascade formed by calcium carbonate precipitating from spring water. The surrounding Szalajka Valley is a protected landscape area within Bükk National Park. Visitors reach the waterfall via a maintained gravel forest road that runs through the valley. The feature is situated in a karst landscape characterized by rich deciduous forests and high biodiversity. The cascading water spans approximately 17 meters in width and height. It serves as a primary geological landmark within the Szalajka-völgy protected zone.
The wooden footbridge directly facing the lower tiers of the waterfall.
Wear sturdy, closed-toe walking shoes as the trail surface is uneven gravel.
Carry a reusable water bottle, as the local spring water is high quality and accessible along the route.
Plan for extra time to explore the nearby Istállós-kő Cave, located on a side trail from the main path.
Attempting to climb or step onto the limestone steps, which damages the delicate, porous structure of the tufa.
Stay on marked trails to protect the fragile travertine structures; swimming and climbing on the falls are strictly prohibited.
