岩溶泉也稱喀斯特泉,指在喀斯特地區,地表水滲入由可溶性岩鹽類被溶蝕形成的洞穴後,迅速地以泉的形式出露於地表形成的泉。[2]

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克羅埃西亞采蒂納河源頭深130米的岩溶泉塞蒂納河泉克羅埃西亞語Veliko_vrilo_(Glavaš)[1]

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