루세나‬에서 가장 멋진 ‪20‬개의 천연기념물

The Fuente del Río in Cabra, is a picturesque natural park considered the origin of the Río Cabra. The park combines the natural beauty of a karst spring with landscaped gardens and a diverse tree landscape. It was declared a “Sitio de Interés Natural” in 1929 and today offers recreational areas and picnic areas for visitors. The spring rises at the foot of the Sierra de Cabra, an area with high rainfall and calcareous rock that leads to the formation of such karst springs. The water flows through a series of waterfalls and artificial springs and supplies the entire municipality. The Fuente del Río is part of the “Ruta del Agua” in the Subbética Cordobesa and offers a harmonious interplay of nature and human design. The park is a popular place for locals and visitors who want to enjoy the tranquility and beauty of this unique place. A visit to the Fuente del Río offers the opportunity to experience the natural beauty of the region and explore the origins of the Río Cabra.

A natural area where the Cabra River is born. A natural spring surrounded by vegetation that transmits peace and tranquility. Highly recommended for a break on the route.

Hermitage that still contains the style of a Mozarabic-style cave church in which the amplitude of its façade stands out, making it one of the few monuments of these characteristics in Andalusia.

Outdoor adventure route, passing through the Hermitage of Nuestra Señora de la Fuensanta and the ruins of old mines.

It is located on the outskirts of the municipality and was built between 1544 and 1620. It is a Mozarabic-style cave church in which the breadth of its façade stands out, making it one of the few monuments of these characteristics in Andalusia. .

One of the last meanders of the Genil river before reaching the Malpasillo Reservoir, close to the town of Badolatosa. Space to be there for a while, quietly and enjoying this beautiful landscape!

In this interesting quarry, from Roman times, stones were extracted for use in mills.

A poljé is a large, elongated, flat valley-shaped depression in an area of karst rock. It is formed after a subsidence of the land in which water often stagnates seasonally. In this case, the Bailón river has produced a drainage of it, and in 2012 a pónor also arose through which the poljé drainage also occurs.