Cova de la Reina

Cave with four entrances that, through a series of passages, connect the racó de la Reina with the coastline of the Meda Gran. The upper entrance is a shaft open to the exterior due to the evolution of the slope that connected a primitive infiltration point in the form of an old chimney. These are the remains of a karstic cavity of larger dimensions that has been dismantled by the evolution of the landscape and marine erosion.

The stalagmitic infilling has been very significant. Notable is the large flowstone that occupies the floor of the central part of the cavity (16 m), descending to the O entrance itself. We also find columns, stalagmites and small stalactites that have survived looting and the corrosive action of marine action. In the lower section a re-excavated stalagmitic thickness is the indication of a total infilling of parts of the gallery. In the exterior prolongation of the cavity, a few metres further on, precisely at the end of the cove, we find more layers of stalagmitic coating of what constituted part of the same network.