At this starting point, the Mediterranean woodland takes center stage, with the holm oak as the main actor, but with an important presence of aromatic undergrowth species
At this point, we leave the path slightly to reach a natural balcony that allows us to contemplate the dehesas of Gansino and Aldeagordillo and the rest of the valley
These granite formations, increasingly present since the beginning of the route, are called berrocales and are an example of granite relief shaped by long-term geological processes
This structure is one of the most remarkable Neolithic remains on the central plateau. It consists of a polygonal funerary chamber, delimited by large granite slabs that formed the walls of the tomb
In this final stretch, the holm oak forest regains prominence, with large specimens that have stood for centuries. Some serve as vantage points for birds to watch over their hunting grounds or build their nests.