Estudio geotécnico in Valverde

In Valverde, sandstones, conglomerates and flysch predominate, which generally provides good bearing capacity for conventional foundations, provided that localised areas of alteration or fracturing within these lithologies are avoided. The formations present frequently host perched aquifers and exhibit significant permeability, a factor that can influence the ground’s behaviour under loading actions and the design of drainage systems and management of groundwater in construction projects.

Seismic activity in Valverde shows a notable number of events over recent years, although with a moderate maximum magnitude (Mmax 3.8); this implies that, while the structural risk associated with seismicity is not severe, it should be taken into account in the sizing of major works or those that are normatively sensitive. No problems of karstification or ground expansivity conditions are presented, so the determining factor for geotechnical studies in this municipality lies in the correct characterisation of permeability and the presence of aquifers, especially in relation to the stability and drainage of foundations.