Estudio geotécnico in Vilamarín

In Vilamarín, the dominant substrate is made up of sandstones, conglomerates and flysch, which accounts for the vast majority of the geological profiles in the area. These materials, together with the occasional presence of slates and schists, generally provide good bearing capacity for shallow foundations, although the low permeability may influence the accumulation of groundwater and require suitable drainage solutions in the foundation design.

Seismicity in Vilamarín is moderate, with 14 events over the last 30 years and a maximum recorded magnitude of 2.4, which indicates a low seismic risk for structural engineering. Since the substrate is non-clayey, the risk of expansivity is ruled out, and the absence of karst removes concerns associated with underground cavities. The main factor conditioning the geotechnical study in Vilamarín is the hydrogeological conditions and the correct characterisation of the type of soil in order to ensure the appropriate sizing of the foundation.