Estudio geotécnico in Villalobón

In Villalobón, the geology is dominated by the presence of limestones, dolomites and marbles, accounting for more than 60% of the substrate, which generally provides high bearing capacity for shallow foundations. Secondary deposits include compact gravels and sands, suitable for stable settlements; however, the occasional presence of gypsum, anhydrite and salts introduces potential dissolution zones that require specific geotechnical checks, especially to prevent differential settlement. The availability of extensive, highly permeable aquifers adds advantages in terms of drainage, but it requires a detailed hydrogeological analysis during design.

With regard to seismic behaviour, Villalobón shows notable seismicity with 57 events over the last 30 years and a maximum magnitude of 4, which necessitates appropriate structural consideration, although it is not determinative. The existence of karst in the carbonate materials implies the need for studies prior to foundation construction in order to rule out cavities or instabilities. The absence of clayey substrates rules out risks of expansiveness. Therefore, checks for karstification and the possible impact of gypsum dissolution constitute the fundamental constraints for building projects in Villalobón.