Crater of the extinct volcano of Racos - Persani Mountains | Photos
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Photos of nearby places
Thieves' Cave - Persani Mountains (20 photos) 6.1 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 6.1 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 22.91 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 36.71 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 37.66 km away
Lake Saint Anna is the only well-preserved volcanic crater lake in Eastern Europe. Here are some images from an afternoon outing.
The Heart of Jesus look-out - Lupeni 42.12 km away
Through the mud on Gordon Mountain, above Farkaslaka (Lupeni commune, Harghita county, Transilvania), on a cloudy afternoon, at the end of February. The destination is the Heart of Jesus lookout, nicknamed as Pléhkrisztus (The Tin Christ).
Other places
Mill of the Devils (Moara Dracilor) Tasna Gorge (Cheile Tasnei) 255.68 km away
The Tasna Gorges are located in the Mehedinti Mountains, approximately 15 km from the resort of Baile Herculane. The gorges are part of the Domogled - Cerna Valley (Valea Cernei) National Park.
The Tasna Gorges are located in the Mehedinti Mountains, approximately 15 km from the resort of Baile Herculane. The gorges are part of the Domogled - Cerna Valley (Valea Cernei) National Park.
Lady's Stones Rarau Mountains 157.74 km away
The Lady's Stones represent the heart, the mind, and the soul. The first two only help to understand the world when one possesses knowledge (they can be climbed with rock climbing gear), as emotions and thoughts (the two rock towers) obscure reality (the view).
The Lady's Stones represent the heart, the mind, and the soul. The first two only help to understand the world when one possesses knowledge (they can be climbed with rock climbing gear), as emotions and thoughts (the two rock towers) obscure reality (the view).
Kaya Bunar (Hotnishki Vodopadi, Hotnitsa Waterfall) Hotnitsa 321 km away
The Kaya Bunar Waterfall (Hotnishki Vodopadi) is located 20 km from the city of Veliko Tarnovo in Bulgaria. The waterfall is 30 meters high, and there are several smaller cascades above it.
The Kaya Bunar Waterfall (Hotnishki Vodopadi) is located 20 km from the city of Veliko Tarnovo in Bulgaria. The waterfall is 30 meters high, and there are several smaller cascades above it.
Rudariei watermills Eftimie Murgu 289.33 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.
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.
Devil's Mill Gorge Campulung Moldovenesc 161.14 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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