Estudio geotécnico in Badolatosa

The subsoil of Badolatosa is characterised primarily by the presence of sandstones, conglomerates and flysch, combined to a lesser extent with fine sands, silts and surface water bodies. These formations have an adequate bearing capacity for conventional foundations, although the frequency of impermeable materials and the occasional presence of surface waters may condition drainage and local ground stability. The limestones and dolomites present in lower percentages suggest localised areas of greater hardness or potential for deep foundations when the quality of the materials allows it.

Seismic activity in the municipality is very low, with hardly any event in recent decades and very low magnitudes, which minimises the seismic influence on geotechnical design. However, given the presence of carbonate formations such as limestones and dolomites, there is a risk of karst processes, so it is essential to verify the presence of cavities or zones of dissolution before defining the type of foundation. In addition, as the substratum is non-clayey, the risk of expansivity is ruled out, making the possible development of karst the critical aspect to be studied for any project in the area.