Waterfall under the hill - Persani Mountains - photos
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Photos of nearby places
Thieves' Cave - Persani Mountains (20 photos) 6.03 km away
The Thieves' Cave at Apata is located in the valley of the Tepeu creek, renowned for its outcrop of red clayey limestone, which is very rich in ammonites. A tributary of the stream is formed by the waters of a spring fed by the watercourse coming from the cave's gallery.
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Videos of nearby places
The Cave of Thieves (Pestera Hotilor, Tolvajos) - Apata 6.03 km away
The Cave of Thieves, located in the Olt Gorge at Racos, is situated at the source of the Tepeu creek. From the karst spring that emerges from the cave, one of the branches of the creek originates.
Varghis gorges in winter 21.29 km away
I went out to admire the ice stalagmites (standing icicles) in the Varghis Gorge. Anyone arriving here at the end of winter can observe meter-high ice stalagmites in the entrance area of Meresti Cave (now known as Orban Balazs Cave).
Preacher's Rock - Bodoc Mountains 28.07 km away
In the Bodoc Mountains, west-southwest from the Henter peak, we find a rock formation shaped like a mushroom by erosion, called Preacher's Rock. This 2-meter high rock probably got its name from the pagan Hungarian priests, who preached here in the past.
Saint Anne lake - Ciomat-Puturosu 29.67 km away
Lake Saint Anna is the only well-preserved volcanic crater lake in Eastern Europe. Here are some images from an afternoon outing.
Nobody's lake - Miercurea Ciuc 40.37 km away
The passage of time (time lapse), dusk at Nobody's Lake. Miercurea Ciuc and the Sumuleu mountain can be seen in the background.
Other places
The Amphitheater of the Dragons (Amfiteatrul Zmeilor) Baia de Fier 166.51 km away
The Amphitheater of the Dragons is the seventh (2017) via ferrata route in Baia de Fier. It was inaugurated last year, on December 26, 2017, after Christmas.
The Amphitheater of the Dragons is the seventh (2017) via ferrata route in Baia de Fier. It was inaugurated last year, on December 26, 2017, after Christmas.
Rhein Gorge Flims, Switzerland 1243.39 km away
The Rhine River (in German, Rhein) originates in the Swiss canton of Graubünden at the Oberalppass and flows into the North Sea at Rotterdam in the Netherlands after traveling 1,324 km. The Rhine Gorge, also known as the Swiss Grand Canyon (in Romansh, Ruinaulta), winds for 14 km between 350 m high white walls.
The Rhine River (in German, Rhein) originates in the Swiss canton of Graubünden at the Oberalppass and flows into the North Sea at Rotterdam in the Netherlands after traveling 1,324 km. The Rhine Gorge, also known as the Swiss Grand Canyon (in Romansh, Ruinaulta), winds for 14 km between 350 m high white walls.
The Cave of Thieves (Pestera Hotilor, Tolvajos) Apata 6.03 km away
The Cave of Thieves, located in the Olt Gorge at Racos, is situated at the source of the Tepeu creek. From the karst spring that emerges from the cave, one of the branches of the creek originates.
The Cave of Thieves, located in the Olt Gorge at Racos, is situated at the source of the Tepeu creek. From the karst spring that emerges from the cave, one of the branches of the creek originates.
Buzludzha monument Kazanluk 366.13 km away
Buzludzha is a historically significant mountain located in the Central Balkan Mountains of Bulgaria. At its summit, at an altitude of 1432 meters above sea level, there is an abandoned monument.
Buzludzha is a historically significant mountain located in the Central Balkan Mountains of Bulgaria. At its summit, at an altitude of 1432 meters above sea level, there is an abandoned monument.
Devil's Mill Gorge Campulung Moldovenesc 161.1 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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