bulgaria smolyan lakes |
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navigate by keyword : and are black bulgaria contact decreases formed from lakes landslide large left mount occipital orpheus resulting rhyolite river rocks scattered sedimentary slope smolyan snow the them they town underneath valley waterproof |
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They are scattered on the left slope of the valley of the Black River , from the Orpheus rocks and Mount Snow to the town of Smolyan. Formed in the occipital decreases in large landslide resulting from the contact of the rhyolite rocks underneath them waterproof sedimentary rocks. |
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