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Updated: May 17, 2025
The range in the Crimea from Cape Kersonese to the Bay of Ratla is formed of layers of limestone alternating with clay and argilaceous schist, a disposition of the strata that tends greatly to accelerate the disintegration of the cliffs. The clay gradually washed out by springs or eaten away by the weather forms great caverns in the sides, and these are liable to fall in when deprived of support.
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