Like the other municipalities of the region, it is located between the mountain and the Guadalquivir valley. Its fundamental economy is the olive tree, although it has an incipient tourist development

The waterfall is located next to the Falcones (1448 m), mountain always visible from any street of Cazorla, and a natural stone wall "Los Castellones" (1,820 m), elevation as a fortress from where it is named. To appreciate the water leaps it will be necessary to climb up a narrow path that runs next to the slope of the stream where you will be accompanied by the cornicabra (Pistacia terebinthus), a very abundant species on this path. By moving along the path you will appreciate the impressive fall of water as soon as the limestone walls serve as slides.

We suggest:

• Next to the bridge from where the waterfall is seen, a right-hand road leads us to the control of Riogazas. It is a pleasant walk in which you will find a fountain called "The River" and another beautiful waterfall, that of the Magdalena. From here goes down a road to Cazorla.

In the Iruela you have to reach the square of the City Hall from where the road ascends towards the hotel Riogazas. 5 km from the Iruela and after two lookouts with meringeros there is a bridge. To the left we can see the Cascade of the Escaleruela.

Information and Observations

• We will have to leave the vehicle at the entrance of the lane because there is a barrier to avoid the passage of vehicles.
• The property through which the lane passes is private so it is not allowed to enter the lane with vehicle.

The upper part of the Borosa River, has a scalated profile for the development of pozas and waterfalls in which travertine terraces are formed with spectacular botroidal calcite morphologies that were precipitated during the most humid and warm periods of the Quaternary.

Although travertine appear throughout the river, the highest concentration is located in the sector between the organ jump and the electric power plant. Its formation is due to the precipitation of calcite caused by the tear-up of the river waters produced by the turbulent regime of the water leaps in the areas with the greatest slope. This precipitation occurs in areas of dense vegetation receding elements of plants and producing subvertical sheets known as cascade facies.

The infant Charles III, son of Philip V, in one of his travels, stayed in this palace on October 27, 1731, then the infant Charles III, King of Spain from 1759.
He stayed in this palace to avoid an outbreak of smallpox plaguing Andújar.
In the afternoon he was distracted by hunting from his window and at nightfall he witnessed from the windows of his room the artefacts that were prepared for such an occasion in Andújar.

In Beas de Segura we find different examples of this type on Feria Street. In Orcera we find some interesting houses on San José Street or in Genaro de la Parra. In the Gate of Segura and in Siles there are also examples of this architecture called generally regionalist, but what they are looking for at the bottom is to incorporate elements from other times in the design of the houses.

Elements of Muslim architecture will give rise to the ne- mudejar and so during different times as the rebirth or the baroque. Its owners intended to legitimize their situation of being able to recover elements of the medieval or Renaissance past, as an element that would serve to connect with the nobility and thus justify their situation of power. To talk about this type of construction, is to make it from the 19th century, a century of great transformations, a time in which the saws that make up the Natural Park know the province of Jaén and the establishment of mechanism and forms of government totally different from those that exist with the advance of Cazorla and the envination of Segura. It is the century in which great fortunes are formed and at the same time the number of poor families is growing exponentially, all of which are framed in a constitutional regime that is completely unknown to most of the inhabitants.

The House of the Chains is a three-storey construction that offers a compact and solid image highlighting Renaissance elements such as the half-point arches. A large entrance arch contains the shield of the Godoy family, the first owners to be recorded.

In particular this stretch of road runs almost air in the interflude of the valleys of the Guadalimar and the Guadalquivir. From this area you can see thousands of hectares of olive trees in a single look, framed by the horizons of Sierra Morena on one side, and Sierra de Segura and Sierra de Las Villas on the other.

The stratigraphic section of Cabañas is a mandatory reference of the Jurassic to Cretaceous transit in the Prebetic Zone. The materials that apflorate are essentially carbonates, in which the tidal levels stand out with marked cyclicity and magnificent examples of surfaces with drying cracks.

Reef faces, levels of accumulation of ferruginous oils, and limestones with spectacular sedimentary structures caused by traction currents are also observed. In addition to the section itself, the panorama contains an example of angular discord between the Jurassic materials and various Cretaceous terms of high paleogeographic interest.

Source: Inventory of Georresources of Andalusia. Environmental Council. Junta de Andalusia.