Estudio geotécnico in Alcaudete

In Alcaudete, the predominant soils are sandstones, conglomerates and flysch materials, accompanied by frequent outcrops of limestones, dolomites and marbles. These lithologies usually offer good bearing capacity, which may facilitate the adoption of shallow foundations, especially on formations of compact rock. The presence of dispersed fine sands and silts is marginal in the distribution, but it is important to correctly identify areas of low cohesion or high porosity. The presence of groundwater bodies indicates the possible existence of shallow aquifer horizons, which is relevant for the design of drainage on site.

Seismic activity in this area is moderate, with 34 recorded events over the last 30 years and a maximum magnitude of less than 4.5, so the seismic influence on structural design is not relevant. The non-clayey substratum rules out the risk of problems due to expansivity. Given the notable development of carbonate formations, it is essential to verify the presence of karst cavities before executing any foundation, as they could compromise the stability of the works. The geotechnical study in Alcaudete should focus mainly on assessing karst features and local groundwater levels.