Stan Valley Canyon - video
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.
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Photos of nearby places
Circular hiking tour in Cozia Mountain (48 photos) 22.33 km away
Arutela - Turnu monastery - Rosiei Rocks - Turneanu ridge - Cozia peak - Stone portal - Stanisoara monastery - Gardului waterfall.
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Videos of nearby places
Stan Valley Canyon in winter 1.13 km away
The Stan Valley is a picturesque canyon, even in winter. In fact, when the stream is frozen and covered with a layer of snow, exploring the canyon becomes much quicker and easier.
Poenari citadel - Arges valley 1.71 km away
The Poenari citadel is located on the southern slope of the Fagaras Mountains, on the western side of the Transfagaras road, in the Arges Valley, about 4 km from the Vidraru Lake dam. Along a steep incline, a concrete staircase leads up to the castle, which is built atop a mountain.
Doabra Stones - Brezoi, Lotru Mountains 28.99 km away
The DN7A road branches off west from the Olt Valley, from the main road between Sibiu and Ramnicu Valcea, leading towards Voineasa and Lake Vidra. The first settlement is a small town, Brezoi, which is located at the confluence of the Lotru and Olt rivers.
Snow-covered valley of Balea and the Transfagarasan in winter - The ascent 30.59 km away
The Fagarasi Mountains can be easily approached from the north, mainly by using the Transfagarasan Road. This high altitude mountain road is only accessible during the summer months (throughout its entire length), but from the Balea Waterfall station (Statia Balea Cascada) you can also reach the Balea Lake by cable car.
Other places
Corcoaia Gorge Gorj county 152.63 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.
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.
Hodoaba Valley iron path Suncuius 236.36 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.
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.
Schulter Anstieg klettersteig Hoher Dachstein 874.91 km away
Two routes lead to the top of the Hoher Dachstein. The Randkluft is shorter, but can only be reached through a glacier with cracks.
Two routes lead to the top of the Hoher Dachstein. The Randkluft is shorter, but can only be reached through a glacier with cracks.
Balázs Hill Lookout Western Mecsek 509.1 km away
The Balázs hill lookout, located at an altitude of 320 meters, offers a beautiful view of Lake Pécs and the wooded mountain ranges of Western Mecsek. The original lookout, built in 1975, was destroyed by fire, and it was rebuilt in 2001 using a metal structure, which was renovated in 2014.
The Balázs hill lookout, located at an altitude of 320 meters, offers a beautiful view of Lake Pécs and the wooded mountain ranges of Western Mecsek. The original lookout, built in 1975, was destroyed by fire, and it was rebuilt in 2001 using a metal structure, which was renovated in 2014.
Devil's Mill Gorge Campulung Moldovenesc 247.04 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.
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.
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