Videos of nearby places
Black Rocks iron path - Bihor Mountains 6.25 km away
Black Rocks is located in the Bihor Mountains, near the Vartop Saddle, to the west of it. It is interesting that the locals (if I understood correctly) do not know this name, but use the name Piatra Buna (meaning Good Stone) for this spectacular rock.
Meziad cave - Padurea Craiului Mountains 24.26 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.
Crystal Cave at Farcu Mine 31.34 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.
Hodoaba Valley iron path - Suncuius 42.14 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.
Other places
Hot air balloon parade 2015 Campu Cetatii 186.32 km away
This year, the Hot Air Balloon Parade was organized in Campu Cetatii for the tenth time. Unfortunately, the weather only allowed for flying on Saturday morning and evening.
Bolii Cave Banita 135.33 km away
The Bolii Cave is located 6 km north of Petrosani, on the road that connects Hateg with the Jiu Valley. Here, the railway line that connects the two parts of Hunedoara County passes through, featuring a total of 66 curves and 8 tunnels.
The Bear's Jump iron path Baia de Fier 177.13 km away
The Bear's Jump (Saritoarea Ursului) is a fantasy-named via ferrata that opened in May 2018 near Baia de Fier, alongside the Middle Belt (Spirala Medie). Both routes begin from the G zone of the rock face that conceals the Women's Cave (Pestera Muierilor).
Devil's Mill Gorge Campulung Moldovenesc 252.31 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.