The waterfalls are formed by the Mirusha River, a tributary of the White Drin.
The series of waterfalls spans a total length of approximately 10 kilometers along the canyon.
The water contains high levels of dissolved minerals, contributing to the distinct turquoise hue of the pools.
The terrain is characterized by karst topography, resulting in frequent formation of caves and grottos nearby.
The site remains a geological interest point due to the active deposition of travertine.
Mirusha Waterfalls consists of a series of 16 cascades and lakes carved into a canyon by the Mirusha River. The waterfalls flow over limestone and gypsum rock formations, which create distinct travertine terraces. The area is part of a protected nature reserve in central Kosovo known for its geological significance. The largest waterfall measures 22 meters in height, feeding into a deep swimming hole at its base. The river creates a natural bridge and several smaller subterranean passages due to the karst terrain.
The ledge overlooking the main central waterfall provides a clear view of the cascading tiers.
Wear water shoes with good grip, as the limestone rocks near the water edges can be slippery.
Bring a waterproof bag for electronics, as the spray from the cascades is significant.
Carry your own drinking water, as facilities on-site are limited or non-existent.
Do not attempt to climb the wet limestone rocks surrounding the falls, as they are prone to crumbling and are very slick.
Pack out all trash to maintain the protected status of the nature reserve; do not use soaps in the swimming holes.
