Estudio geotécnico in Trijueque

In Trijueque, the subsoil is composed mainly of limestones, dolomites and marbles, with a secondary presence of sandstones, conglomerates and flysch. These materials, with low permeability at the surface, normally provide good load-bearing capacity, suitable for most buildings, although the eventual presence of deep aquifers may influence the choice of the foundation system and the management of groundwater.

Seismic activity in the municipality is very low, with barely a single recorded event in the last 30 years and a clearly low maximum magnitude, which minimises the need for seismic adaptations in the structure. That said, the karstic nature of the ground requires checking for the possible existence of cavities or voids before carrying out the foundation, as this constraint can be decisive for the safety and stability of the building. In this area, the absence of clayey soils rules out the risk of expansivity.