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Abstract
We propose a possible model of genesis of the cluttered boulders and pseudokarstic caves, of which one is the famous St. Teodora’s cave, in the area of Sihla Skete, an important spot of tourism and Ortodox pilgrimage. Our model takes into consideration the entire geologic history of the area, beginning with the deposition of the sedimentary rocks on which the peculiar relief of the area is sculpted to present day.
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