Estudio geotécnico in Cenicientos

In Cenicientos, the predominant geotechnical subsoil is mainly composed of granite, gneiss and other igneous rocks, accounting for more than 94% of the soil types found in the area. These rock formations are highly solid and have very low deformability, which guarantees excellent bearing capacity for buildings. Compacted gravels and sands, although infrequent, may occur locally and also provide good conditions for foundations. In general, the surroundings offer favourable conditions for direct foundations, typically shallow or semi-deep, founded on consistent strata.

The recorded seismicity in Cenicientos is very low, with just five events over thirty years and a maximum magnitude of 3, which means it does not represent a relevant constraint in structural design. Since there are no risks associated with karstification or expansive soils, and the non-clayey subsoil rules out the possibility of expansivity problems, the main factor to take into account will be the potential presence of shallow groundwater levels in specific areas, although the overall geotechnical risk is low.