Estudio geotécnico in Torija

In Torija, soils formed by limestones, dolomites and marbles predominate, reaching almost 73% of the surface, while sandstones, conglomerates and flysch account for a little over 22%. These substrates usually provide good bearing capacity for shallow and deep foundations, although their low surface permeability may condition the disposal of water, and at depth significant aquifers may exist that need to be controlled in the foundation design.

Seismicity in the area is very low, with a single event with a maximum magnitude of 1.7 over three decades, which does not imply any specific requirements for structural design. However, the presence of carbonate materials makes it essential to verify the possible existence of karst cavities before carrying out foundation works, as they can generate localised instability. Since the substrate is not clayey, the risk of expansivity is ruled out as a determining factor for the geotechnical study in Torija.