Polje de la Nava
A polje is a large, enclosed, elongated depression with a flat floor found in karst terrain.
This polje has both tectonic (involving a thrust fault and subsidence of the land) and karstic (rock dissolution) origins. It lies at an altitude of around 1,000 metres and is of medium size among the poljes of Andalusia, measuring 7 km in length and 1 km in width. For much of the year, water drains into the subsoil in a diffuse manner, through cracks in the floor and via a sinkhole that suddenly appeared in 2012. During the rainy season, due to the low permeability of the clays at the bottom, La Nava de Cabra tends to flood, and on occasions the sinkhole is unable to cope with the volume of water and becomes submerged.
Polje de la Nava
A polje is a large, enclosed, elongated depression with a flat floor found in karst terrain.
Dive
A ponor is an opening through which surface water (from a river or lake) flows wholly or partly into a karst groundwater system.
The waterfalls
Waterfalls located near the polje
Paleodolina
A doline (a word of Slovenian origin meaning ‘valley’ or ‘depression’) refers to a specific type of geological depression characteristic of karst landscapes....
Fuenfria
A spring that supplies drinking water to the people of Zuheros.
Bailón River Gorge
Along with the Nava polje, it is one of the most characteristic karst features in the Sierras Subbéticas Natural Geopark. Over thousands of years, the action...
Fraile's Cave
The cave takes its name from a cluster of stalagmites that resembles a monk’s hood.
The Portillo Alto Era
An agricultural site designed to separate the grain from the rest of the plant.