Estudio geotécnico in Los Santos de Maimona

In Los Santos de Maimona, formations of slates and schists predominate—materials of metamorphic nature that provide a competent substrate with low permeability. These characteristics usually translate into a good bearing capacity for most buildings, although it is essential to study the possible presence of fracturing and surface alteration, as well as the variability in the depth of the optimum foundation levels.

The area shows notable seismicity, with 52 events over the last 30 years and a maximum magnitude of 4.4, which advises that seismic action should be considered in the structural design of buildings. In addition, due to the potential presence of karstification in the substrate, it is essential to verify the existence of cavities or dissolution processes before carrying out any foundation work in order to avoid future defects. The absence of expansive clays implies that there is no risk of expansivity associated with the soils, with the karst assessment remaining the main local geotechnical constraint.