Abstract
Travertine springs (petrifying springs) are unique natural formations formed by a complex interaction of abiotic and biotic factors, which cause the precipitation of calcium carbonates and magnesium from solutions saturated with corresponding hydrocarbonates. This is how travertines are formed (another name is limestone or freshwater tuffs) - specific carbonate rocks of the sedimentary type, common in continental bodies of water - springs, streams, lakes, etc.
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