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This castle stands on the impressive Alacranejo hill and, despite its original defensive character, it underwent various modifications. Opposite it there is another hill with the ruins of the Salvatierra Castle, in the lands of Calzada de Calatrava. It probably has Arab origins, but it was deeply remodeled with the transfer of the knights of the Order from the Castle of Calatrava La Vieja (Carrión de Calatrava) in 1217, after the battle of Las Navas de Tolosa with the aim of consolidating the defensive line of Sierra Morena. In turn, it is made up of three walled enclosures and is accessed by the original road that was built on the occasion of the visit of Philip II through the Iron Gate, in red volcanic stone. Afterwards, we can find the Gate of the Arches, which allows entry into the parlatorio or courtyard of the convent, the courtyards, the church, the rooms and the refectory. Really, when you walk through it, you can imagine what happened in
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The Fuente Agria is one of the most emblematic icons of Puertollano. Located on the Paseo de San Gregorio, this fountain is known for its water with a high iron content, which gives it a characteristic flavor and health benefits.
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The Ruta del Mercurio in Alcolea de Calatrava is a fascinating hiking route that takes you through unique volcanic and natural landscapes. This route stands out for its geological wealth and its mining history, as the area was known for the extraction of mercury in the past.
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Puente Morena is a prominent place on the Jabalón River, in the province of Ciudad Real. It is known for its hydrological monitoring station, which is part of the Guadiana River basin. This station collects important data on water flow and other hydrological parameters. Additionally, Puente Morena is significant for its geological characteristics. It offers a classic Upper Ordovician stratigraphic section, showing three different units: Mixed Banks, Urban Limestone and Chavera Slates2. This makes it an interesting site for geological and paleontological studies.🌄🚴😎
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It is formed by a Strombolian volcanic cone of pyroclasts, and due to the quarry in it, its internal structure is exposed. Attached to the foot of this volcano is the Almodóvar maar, which is a phreatomagmatic explosion crater that erupted at the edge of the Paleozoic series, cutting a substrate of hard lithology and destroying part of the previous volcano. The maar crater is funnel-type (hard-type substrate) and houses an ephemeral lagoon inside. In its southern and eastern contour the maar has a ring of tuffs, with pyroclastic facies. The phreatomagmatic deposits of the maar ring are located on a Cenozoic red colluvium. The main interest is of a volcanological (petrological) type and as a secondary interest the geomorphological interest stands out.
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Settled on a fortified hill that has dominated since the Bronze Age, controlling the Port of Calatrava, a natural route to the Sierra Morena from the southern Spanish Plateau. The Castle and Convent of Calatrava la Nueva are monuments from the 12th century of great importance. Spectacular views from the top over the surrounding landscape.
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