The waterfall is built of travertine, a form of limestone deposited by mineral-rich springs.
It is one of the few waterfalls in Slovakia located within the immediate urban footprint of a village.
The water source is a powerful karst spring known as 'Vyvieračka pod Hrhovským hradom'.
The deposit formation at the site is active, meaning the waterfall's structure is constantly evolving through mineral precipitation.
The area is part of the buffer zone for the Slovak Karst National Park, a UNESCO World Heritage site.
Hrhov Waterfall is a travertine cascade situated in the village of Hrhov, Slovakia, fed by a strong karst spring flowing directly from the Slovak Karst plateau. The waterfall drops approximately 15 meters over a unique tufa formation, which continues to grow due to the high mineral content of the water. Unlike many waterfalls, it is located within a residential area, directly adjacent to local private properties and a village road. The water flow is perennial, though volume varies significantly based on precipitation. The site is a protected natural monument designated to preserve its geological and geomorphological value. It sits at the foot of the Hrhovska vyhliadka, which offers views over the Bodva Basin.
From the small footbridge or the roadside viewpoint directly facing the falls.
Park in the designated village areas and walk to the waterfall to avoid obstructing local traffic.
Visit after periods of heavy rainfall to see the water cascade with maximum intensity.
Respect the privacy of the local homeowners whose properties directly border the waterfall area.
Do not attempt to climb the travertine cliff face, as it is fragile and slippery.
Keep noise levels low and stay strictly on marked paths to protect the fragile travertine formations.
