Top 20 Natural Monuments around Pozuelo De Calatrava

It is located next to the town centre of Pozuelo de Calatrava. It is popularly known as the unexpected lagoon. If you pass by, it is a unique opportunity to enjoy the flora and fauna of the saltiest lagoon in the area.

La Hoya del Mortero is one of the maars that best preserves its structure in Campo de Calatrava. Its crater forms a depression about 30 meters deep and about 500 meters in diameter. To appreciate these dimensions, it is best to visit it and observe it from its edge. Currently there is an interpretive panel from which we have a good view of the whole and helps to understand what we are seeing. Starting point of the Ciudad Real Greenway.

Small lagoon that is very close to the center and what's more, the path that goes around it is quiet and pleasant close to the center.

The so-called “hotbeds” are one of the most common phenomena in the Calatrava region, as a consequence of its intense volcanic activity. A unique spectacle that, together with sour springs, maares, wells, and jets or sinas, are part of the history of the region and that the Association for the Development of Campo de Calatrava tries to preserve and make known outside its borders.

Within the Campo de Calatrava region, this municipality attracts the visitor's attention because it is close to two salty lagoons of volcanic origin, Argamasilla and Inesperada; formerly used as medicinal waters. Like other thermal springs where the Infante Don Carlos ordered the construction of the Baños de Fuensanta. In addition to its natural assets, the religious ones are important, in the form of a church and a sanctuary that we must not miss. Its 17th century church dedicated to Saint John the Baptist was declared a B.I.C. in 1989. Its nave is covered by a barrel vault and has a polygonal apse and two doorways under porticoes, one of them with Tiara Papal. It is one of the few churches that preserves its three original altarpieces from the 18th century, the most important being that of the High Altar made of walnut wood without polychrome and with allegories of the Trinity. In the Sanctuary of Nuestra Señora de los Santos we can also admire a beautiful altarpiece in Churrigueresque forms. The sanctuary is on the outskirts of the town and was built on an old Arab fortress. It has a single nave in which we will see wall paintings and a beautiful Mudejar coffered ceiling.

Pozuelo de Calatrava is a rustic town of medieval origin located in the historic region of Campo de Calatrava, on the edge of one of the most interesting volcanic lagoons in the territory: La Inesperada or Laguna del Prado, where you can spot various waterfowl.

Within the Campo de Calatrava region, this municipality attracts the visitor's attention because it is close to two salty lagoons of volcanic origin, Argamasilla and Inesperada; formerly used as medicinal waters. Like other thermal springs where the Infante Don Carlos ordered the construction of the Baños de Fuensanta. In addition to its natural assets, the religious ones are important, in the form of a church and a sanctuary that we must not miss. Its 17th century church dedicated to Saint John the Baptist was declared a B.I.C. in 1989. Its nave is covered by a barrel vault and has a polygonal apse and two doorways under porticoes, one of them with Tiara Papal. It is one of the few churches that preserves its three original altarpieces from the 18th century, the most important being that of the High Altar made of walnut wood without polychrome and with allegories of the Trinity. In the Sanctuary of Nuestra Señora de los Santos we can also admire a beautiful altarpiece in Churrigueresque forms. The sanctuary is on the outskirts of the town and was built on an old Arab fortress. It has a single nave in which we will see wall paintings and a beautiful Mudejar coffered ceiling.

The Prado Lagoon is a saline volcanic lagoon with seasonal waters, located in the municipality of Pozuelo de Calatrava. Hydrographically it belongs to the Guadiana river basin. Its origin is pseudokarstic, since it was caused by a phreatomagmatic explosion at a fracture junction located in a sedimentary basin. This has favored surface ponding like this semi-arid lagoon, with sulphated-magnesium-sodic chloride waters. Due to its salinity, the vegetation is relegated to the margins, mainly salt marshes and halonitrophilous plants. The contribution of rainwater from the town has altered that salinity, allowing the appearance of reeds, castanets and even white poplars. During periods when it is flooded, you can see black-headed gulls, black-headed gulls, avocets, stilts and plovers, as well as pink flamingos.