Geoparque Mundial UNESCO

Nº08 – Hornos de la Calera Alía

Geoparque Villuercas > Nº08 – Hornos de la Calera Alía


La Calera is a hamlet of the village of Alía. It can be reached by a local road about 10 km north of the centre of Alía.

Some six kilns are still standing in various states of conservation. The ovens and the limestone quarries can be seen. The kilns are located in two groups:

The first of them in the vicinity of the village, taking the road to Navalvillar de Ibor. It is made up of a group of three kilns, one of which is practically destroyed, and a fourth which is separate from the first three.

The second group of kilns, and the most distant, is also in relatively good condition and, as in the previous group, the quarries for extracting limestone rocks are located nearby.

To complete your knowledge, we recommend a visit to the La Calera Kilns Interpretation Centre, located in the village centre, which shows the process of extracting limestone rocks in the quarries and the subsequent production of lime in the kilns.


The origins of this small village are due to the quarries and lime kilns in the surrounding area, which were used at different times, above all to supply lime to the nearby Monastery of Guadalupe during its construction in the 14th century. Next to the kilns can be seen the quarries from which the limestone rocks were extracted. The quarrying face can be seen, which is about 3 m high and 25 m long, with the largest area of these rocks covering almost 100 m2.

The dimensions of the kilns are almost uniform, with a diameter of 2.5 m and a height of 3-3.5 m. The limestone (calcium carbonate, CaCO3) was placed on a bed of holm oak wood. They were lit and subjected to calcination, at a temperature of 700-900ºC for three days, in order to convert the calcium carbonate in the limestone into quick lime (calcium oxide, CaO). The quicklime is slaked by adding water and a white paste is obtained which is used to whitewash walls and as a binding element, mixed with sand, to build stone or brick walls.


From a geological point of view, these carbonate outcrops belong to the Ibor Group, from the Ediacaran period, which outcrops extensively in the geopark. The most extensive outcrops are located on the flanks of the great Ibor anticlinorium, disconnected from each other as they are arranged in an “beaded” fashion.

In terms of their origin, they are chemical precipitation deposits and bioconstructions of microbial mats (stromatolites) formed in shallow marine environments during the Ediacaran period.

To the southwest of the quarries, the wide valleys are dominated by the shales and greywackes of the Guadiana Formation (Domo Extremeño Group), over which the Ibor Group is discordant. On the slopes, crowned by the Armorican Quartzite, are the limestones, shales, sandstones and conglomerates of the Ibor Group, largely covered by the typical rocks of the Sierra Palomera.