周辺のスポット/アトラクション・トップ20

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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On the hill of Cerro de los Molinos you can see the ruins of an old windmill built in the 18th century, near the old castle, which is why this place is popularly known as El Castillo. The historic castle was a fortress with four stone towers, surrounded by high walls and thick walls, with a moat around it, built during the Islamic domination of the Peninsula. These data are known from historical documents, but there are no current vestiges of their presence.

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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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On the hill of Cerro de los Molinos you can see the ruins of an old windmill built in the 18th century, near the old castle, which is why this place is popularly known as El Castillo. The historic castle was a fortress with four stone towers, surrounded by high walls and thick walls, with a moat around it, built during the Islamic domination of the Peninsula. These data are known from historical documents, but there are no current vestiges of their presence.

Googleによる翻訳•原文を表示

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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On the hill of Cerro de los Molinos you can see the ruins of an old windmill built in the 18th century, near the old castle, which is why this place is popularly known as El Castillo. The historic castle was a fortress with four stone towers, surrounded by high walls and thick walls, with a moat around it, built during the Islamic domination of the Peninsula. These data are known from historical documents, but there are no current vestiges of their presence.

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Located at the foot of the Monument to the Miner, an imposing bronze sculpture, the work of Pepe Noja, which represents the mining history of the city, borders the volcanic area of Campo de Calatrava and in its vicinity is the Valley of Alcudia. Mining activity is of special importance with the Mining Museum, a building that surrounds an old headframe and simulates a coal selection workshop. On its two floors, the museum discourse addresses the transformation of Puertollano into an industrial city due to the discovery of coal. The mining tradition of this town is very present in its different corners, such as the Castillete de Santa María, which welcomes its visitors at the entrance to the city. It is also worth seeing the Monument to the Miner, mentioned above and located on the Cerro de Santa Ana, from which we will obtain a fantastic panoramic view of the city and its surroundings.

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This castle stands on the impressive Alacranejo hill and, despite its primitive defensive character, it underwent various modifications. In front of it there is another hill with the ruins of the Salvatierra Castle, in the lands of Calzada de Calatrava. It probably has Arab origin, 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 line defense 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 Felipe II through the Iron Gate, in red volcanic stone. Later, we can find the Puerta de los Arcos, which allows us to enter the parlatorio or courtyard of the convent, the parade ground, the church, the rooms and the refectory. Really, when going through it, you can imagine what happened in those medieval times of fights and prayers, as well as enjoying and expanding your heart with the relaxing landscapes that can be seen from its battlements.

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