Phreatic conduits at different leves (Cueva del Agua).
To describe the enormous variety of the caves in the Sorbas Karst would be almost impossible, due simply to their large number. We have preferred to choose just three representative caves: La Cueva del Agua because of its galleries of freatic origin, the Covadura System as an example of interstratified karst, and the Cueva del Yeso because of the close links between the fluvial and the karstic phenomena that have been identified in its formation.
Phreatic conduits at different leves (Cueva del Agua).