Videos of nearby places
Blasted Rock (Piatra Puscata) hanging path - Cerna Valley 41.52 km away
The Blasted Rock hanging path is located on the geographical right bank of the Cerna River, near the confluence of the Iuta stream, approximately 20 km from Baile Herculane. In this area, the presence of limestone formations has caused the valley to become narrower.
Corcoaia Gorge - Gorj county 50.49 km away
The Corcoaia Gorge is one of the most beautiful tourist attractions in the Cerna Valley. It can be reached by car, 43 km away from Baile Herculane, of which about 17 km is on a dusty gravel road.
Rudariei watermills - Eftimie Murgu 57.52 km away
I have visited the twenty-two wooden water mills with horizontal wheels, located in the valley of the Rudaria stream, mostly in the rain and under an umbrella. Some of them are still in use today.
Other places
Waterfalls of Lapos creek Bicaz Gorges 333.67 km away
One of the lesser-known attractions of the Bicaz Gorges is the series of waterfalls along Lapos Creek. This creek flows between Cupas Stone and Bardos Stone before eventually merging with Bicaz Creek, forming spectacular waterfalls beneath the Altar Stone.
Fairy Cliff (Peretele Zanelor) via ferrata route Vadu Crisului 255.14 km away
In Vadu Crisului, in the Padurea Craiului Mountains, on the right bank of the Crisul Repede, you can find the newest, in chronological order (2015) the fifth Transylvanian, new type of via ferrata route. I will not count here the traditional iron paths, the high-mountain hiking trails, partly secured with iron cables, or the rock canyons with iron ladders and footbridges.
Iron path in winter Harghita Madaras 292.89 km away
This is already the sixth time I've climbed the via ferrata route set up on the rocky cliffs of Seii Peak near Harghita Madaras. Although the forecast suggests that the weather should be nice, I am greeted by a sky covered in clouds.
Devil's Mill Gorge Campulung Moldovenesc 379.42 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.