Estudio geotécnico in Ronda

In Ronda, soils predominate that are formed by limestones, dolomites and marbles, together with a significant presence of sandstones, conglomerates and flysch. These materials, generally competent in nature, provide good bearing capacities for buildings, although the existence of compact formations such as gravels and sands is uncommon. In general, the low presence of clayey materials and the relatively low permeability make it easier to select direct foundation solutions, provided that a proper prior characterisation of the ground is carried out and the associated aquifers are located.

Seismicity in the area is notable, with 140 events recorded over the last 30 years, although the maximum magnitude observed is moderate (Mmax 3.7), so this aspect must be assessed in the structural design calculation phase. It is essential to verify the presence of karst processes in the substratum, since the possible existence of cavities or dissolution in carbonate zones represents the main constraint in the design and construction of foundations for any urban development in Ronda. The risk of expansivity is ruled out due to the non-clayey substratum.