Estudio geotécnico in Baños de Río Tobía

In Baños de Río Tobía, sandstones, conglomerates and flysch predominate, accompanied by fine sands and silts. These materials form a generally competent subsoil, where bearing capacity is favourable for shallow foundations, although the presence of silts may impose certain restrictions in terms of drainage. The hydrogeology is characterised by the low permeability of the formations, although at deeper levels significant aquifers may occur, which requires attention in excavation projects or deep foundations.

Seismic activity in the municipality is very low, with only a single recorded event in the last thirty years and a low maximum magnitude. There is no impact from karst and no risks of expansivity have been detected due to the absence of clayey soils, which simplifies the geotechnical approach. The most relevant constraint in Baños de Río Tobía will be the correct characterisation of permeability and any potential presence of groundwater on site, particularly in projects with considerable depth.