Transfagarasan, RomaniaCapra waterfall known as Cascada Iezerului, we find between Capra and Cabana Balea Lake, at an altitude of 1690 meters, Arges county.
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Valea Prahovei, RomaniaA natural monument in the Bucegi Natural Park, the Urlătoarea Waterfall is an easily accessible objective, which attracts spectacular waterfalls, the noise made by them and the picturesque landscape.
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Bran Moeciu, RomaniaReserve biogeologica Moieciu on the road, which connects the Upper Moieciu Netherlands. On the creek bank wall Turcu outward from two threads of water which flows in cascades of 15-20 m.
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Muntii Apuseni, RomaniaIadolina Falls is located below the road on the left side of the road, about 6km from the lake bottom. Anything above, all the left side appears another called Bridal Veil Falls.
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Valea Prahovei, RomaniaAfter 1 hour 30 minutes to climb through the forest to get to the waterfall, which is downright spectacular. Besides her you climb on stairs of metal, in some parts of a chain that you support, others have nothing and yo just lean on walls ...
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Moldavia, RomaniaThe Waterfall is located in Mountain Ceahlau Duruitoarea at an altitude 1270 m and is formed on the river that comes from the alpine rupture and flows into Lake Valley and then Bicaz Hermitage.
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Maramures, RomaniaHorse Waterfalls is located near the tourist resort of Borsa, in the NE of Rodna Mountains.
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Banat, RomaniaBigăr Waterfall is part of the Cheile Nerei-Beușnița National Park, in Caraș-Severin county. Bigăr Waterfall is in the Minis Valley, halfway between Anina and Bozovic
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Transfagarasan, RomaniaLocated in the Fagaras Mountains between peaks and Negoiu Moldoveanu, Ramna most famous waterfall.Waterfall Balea puts you ahead of a performance of a surprising beauty.
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Banat, RomaniaVăioaga Waterfall is on the road that leads to Beuşniţa Waterfall and Lake Ochiul Beiului, two of the most important tourist attractions of Banat. The waterfall is found along the Bei River and measures 5-6 m high.
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Banat, RomaniaThese were born through the action of water for millennia in the limestone substrate. The water-dissolved limestone was deposited layer-by-layer along the course of the river, forming limestone tuff, soft and permeable rock that allowed the modeling of countless shapes, mini-dams, water meshes and successive waterfalls.
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