Traditional constructions have only been modified, although the most rewarding is the view that you can enjoy from the village that really constitutes a natural balcony open to an overwhelming landscape in which stands out on the whole Calar del Cobo with the Puntal of the Mass.

If you like them, you can't stop visiting the Umbria, as it's a very good area for the collection of these mushrooms. In addition, a delicious unmarked road leads to the nearby village of Cabeza Gorda, located on the opposite side of a mountain, which is naturally called Morro de Cabeza Gorda.

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.

It is a travertine of hectometric dimensions, located on the southern side of the valley of the Segura River, in a sector very close between the Puntal of the Vultures (1680 m) and the Calar del Pino (1567 m). The travertine, attached to the steep carbonate side of the Cretaceous, has a higher flat morphology, on which the picturesque village of La Toba is located.

In the vertical walls of the travertine there are several karmic resurrections with spectacular water jumps and great beauty carbonate morphologies. Stratigraphically, the uprisings are at the base of the upper Cretaceous dolomies, which constitute the aquifer, on the waterproof levels that belong to the lower Cretaceous.

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

According to the description of several authors, 3? 4? 5? more than a watchtower would be a chastisement. Built in well-trimmed masonry, its plant is cylindrical with a semicircular wall that protects the entrance. It is located in height (about 2 meters above the ground level) and still retains remains of wood lintel from the door and its cap. There must have been a second floor, as inside the tower remains of beams from the wooden roof that separated both floors. It has two overlapping interior rooms and a terrace. The bottom of the tower is solid. The plants were covered with semi-spherical vaults, communicating with a 1.18 meters wide terraced staircase.

In general it is kept in good condition, although a great crack threatens to break it down

Location: To the south of the town, in the natural park of Cazorla, Segura and Las Villas.

Distance: 42 km

Medium: By vehicle, by bike and on foot.

Access route:: On the road A-319 towards La Iruela; at this point, after going 13 km, we will take the Chorro road, then turn away by the horseshoe road leading to Puerto Llano.

La Taberna Museo Restaurante Lagartijo, is a charming tavern dedicated to the tauromaquia and opened in March 1980. In it you can taste an excellent traditional cuisine in a tourist-cultural atmosphere decorated with billboards, photographs and taurine objects. In it, culture, tourism and gastronomy are hand in hand in a typical Andalusian environment.

The property consists of two areas. The Taberna, dedicated to tasting tapas and rations, can be found just after entering. In this atmosphere, you can enjoy a typical tavern kitchen, surrounded by many objects dedicated to the tauromaquia, such as photographs, posters and light suits.

In the interior is the Museum and Restaurant Room, which has a select menu of kitchen recipes, with typical and traditional dishes, where the meats, peas, and especially the confected and baked ones stand out.

The hill of the Poyos de la Mesa is an inverted relief in which the dolomies of the Upper Cretaceous and the limestones of the discordant Miocene on them are affected by a sincerity perfectly visible from the north.

The fold is more tight in the older materials (Cretaceous dolomies), and is more open in the discordants (myocene limestones). Both litological sets flare at the top, very steep, of the relief. Between them there is a well-developed canchal, which marks approximately the axial plane of the fold.

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