Photos of nearby places
Moanei Cave - Padurea Craiului Mountains (58 photos) 14.7 km away. The Moanei Cave (Pestera Moanei) is located on the upper course of the Misid River, on the right side of the Misid Gorge (Cheilor Misidului). The cave has two entrances, one fossil and sloped, while a subterranean stream flows through the active gallery.
Videos of nearby places
Crystal Cave at Farcu Mine 2.6 km away. In the Padurea Craiului Mountains, near Rosia, in the Farcu bauxite mine, in 1987, the miners accidentally discovered a cave. It was filled with crystal-shaped limestone formations.
Meziad cave - Padurea Craiului Mountains 7.6 km away. The Meziad Cave is located near the village of Meziad, 22 km north of Beius, in the Padurea Craiului Mountains. It is one of our first tourist caves, its exploration is associated with the name of Gyula Czárán, cave researcher and writer.
Hodoaba Valley iron path - Suncuius 18.4 km away. The Hodoaba Valley iron path is Romania's shortest and easiest (official) via ferrata route. It is located near Suncuius, in the Padurea Craiului Mountains, on the left bank of the Crisul Repede River.
Vadu Crisului cave 19.7 km away. The Vadu Crisului Cave, with a total length of over 1000 meters, is located in the picturesque gorge of Crisul Repede creek. It consists of a gently meandering, long passage that features an active, stream level next to an upper, fossil level in its first section.
Other places
Mill of the Devils Tasna Gorge 204.4 km away. Mill of the Devils (Moara Dracilor) - Tasna Gorge (Cheile Tasnei). The Tasna Gorges are located in the Mehedinti Mountains, approximately 15 km from the resort of Baile Herculane.
Stan Valley Canyon 234.4 km away. The Stan Valley is located near Lake Vidraru, southwest of it, in the Fruntii Mountains. Those who have visited the Seven Ladders Waterfall will appreciate this canyon, outfitted with infrastructure for tourist accessibility.
Devils Mill Gorge Campulung Moldovenesc 254.3 km away. The Devil's Mill Gorge is relatively short, measuring only 60 to 70 meters in length. It was formed in yellowish-gray-white dolomite by the work of a stream that crosses the gorge, as a result of erosion and the dissolution characteristic of limestone.