Estudio geotécnico in Fuente de Cantos

In Fuente de Cantos, the dominant geotechnical subsoil is formed by slates and schists, metamorphic materials that provide good bearing capacity and exhibit low deformability. The small proportions of clays, hard marls, granite and sandstones do not significantly affect the overall foundation setting, as the main lithologies tend to offer a compact and stable base. Its permeability, very low in essence, may require attention regarding the control of surface water, but it does not usually represent a serious problem for conventional projects.

The municipality shows no evidence of expansive clayey subsoils, so the risk of expansivity is ruled out. Seismicity is very low, with only seven events over 30 years and a low maximum magnitude, so it does not influence the usual structural design. However, the potential presence of karstic phenomena makes it essential to carry out prior verification before executing any foundation, this being the main geotechnical constraint in the area.