Geological description and formations
These caves are mainly formed by calcareous rock, a type of sedimentary rock that is particularly prone to the formation of karst caves. The action of water on this rock over thousands of years has resulted in the creation of this subway complex.
Inside the Caves of Campanet you can observe various geological formations, each with its own beauty and uniqueness:
The stalactites are hanging formations are created by the deposition of minerals dissolved in the water dripping from the ceiling of the cave. In the Campanet Caves, stalactites come in a variety of shapes and sizes, some of them reaching impressive dimensions.
Stalagmites are formations that grow upwards from the cave floor, also formed by the accumulation of minerals deposited by dripping water. In some areas of the caves, stalagmites have joined with stalactites to form columns.
Pillars and pillars are structures formed when a stalactite and a stalagmite grow to meet and merge. The columns of the Campanet Caves are particularly notable for their thickness and height, some of which appear to support the ceiling of the cave.
Curtains and trays are less common formations that form when water flows down a sloping surface or over the edge of an existing formation. In the Campanet Caves, these structures add an extra dimension of beauty, with their delicate shapes and translucent colors.
Finally, pools of water containing crystalline water can be found in various parts of the caves, formed by the constant dripping of water. These pools reflect the cave formations, creating an impressive visual effect.
The combination of these formations creates a subway landscape of almost surreal beauty. The variety of shapes and sizes, along with the play of light and shadow, make the Campanet Caves a place of wonder and admiration, where every corner reveals a new aspect of nature’s majesty.