Batca Mica - Hasmas Mountains | Photos

Lonely Stone (Piatra Singuratica) - Hasmas Mountains 4.29 km away
On June 1, 2003, with a small group of friends, I left Balan, walking along the valley of the Sep (Beautiful) stream towards the Lonely Stone (Piatra Singuratica). Those who were with me at the time fell behind, and then other people joined for the hike.

Wild Ferenc iron path - Suhardul Mic 9.19 km away
While I climbed the new iron path mostly in the dark for the first time, this time I managed to explore it during the day. But I still missed the sunset by a few minutes.

Wild Ferenc memorial path - Suhardul Mic 9.21 km away
In recent days, this news has been everywhere: the via ferrata route built on the southwest wall of Suhardul Mic (Little Suhard) has finally been completed and inaugurated. The new route has been named after Ferenc Wild, in memory of the former mountain rescuer, sports writer, and one of the founders of the mountain rescue association in Gheorgheni.

Poienii Rock, north-eastern lookout point - Bicaz Gorge 10.66 km away
From the viewpoint at the top of the northeastern wall of Poienii Rock in the Bicaz Gorges, we can look down 300 meters to the mouth of the Bicajel stream. The Bridge of the Hungarians is hidden among pine trees.

Bicajel Gorge (Cheile Bicajelului) - Hasmas Mountains 10.68 km away

Pietraru pottery Horezu 222.94 km away

Piticot iron path for children Suncuius 248.24 km away

Crystal Cave at Farcu Mine 256.87 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.

Ski resort Poiana Brasov Postavarul Mountains 128.53 km away
Shining sun and an Austria-feeling on the impeccable slopes of the ski paradise Poiana Brasov above Brasov. Sunbathing, coffee and refreshing drinks on the terrace of Julius Römer chalet.

Devil's Mill Gorge Campulung Moldovenesc 85.52 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.

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