The ravine of the Valhondo stream was the usual communication channel between Pezuela de las Torres and the towns of Nuevo Baztán and Olmeda de las Fuentes, a fertile plain …
The relief of the Tajuña valley is the result of a succession of horizontal sedimentation processes during cold and dry periods and a strong erosion by water and the elements, …
The little valley of the Dehesilla stream transmits distance and solitude, it is a valuable portion of wild mountain hidden and concealed between the slopes of the moor and the …
The small gravel and sandstone slopes in the upper section of the Valdemembrillo stream are very eroded and reveal the geological soil of the territory that originated 25 million years …