Czech limestone country spans two geologically distinct zones — the Moravian Karst north of Brno, and the Bohemian Karst west of Prague — separated by the Bohemian Massif and shaped over hundreds of millions of years.
Both regions formed in ancient marine sediments. The Moravian Karst rests on Middle Devonian limestones roughly 380 million years old. The Bohemian Karst contains even older Silurian and Devonian strata, with some outcrops exceeding 400 million years. Surface water percolating through fractures gradually dissolved the bedrock, forming the cave corridors, pits and underground river systems visible today.
The Czech Republic registers more than 1,100 catalogued cave cavities. Of these, six cave systems in the Moravian Karst and one in the Bohemian Karst are administered for public access by the Czech Cave Administration (caves.cz), which oversees visitor access, scientific research and conservation measures.
Beyond the two major karst zones, isolated limestone outcrops appear in Moravia near Zbrašov (with its CO₂-rich thermal caves) and in the Jeseniky highlands. Smaller karst windows also occur along the Dyje River valley in the Podyji National Park.