 Most of the terrain in the Kornati islands is karst-limestone which, in the distant geological past, arose from sediment from the sea. In the stone on the islands there are numerous fossils of crustaceans and fish. In the area there examples of all the typical forms of karst: bizarre shapes formed by the atmosphere, unexplored caves, areas of flat rock and, above all, cliffs. Karst rock is porous, rapidly draining and dry, and so therefore are the Kornati islands.
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