Estudio geotécnico in Palomares del Río

In Palomares del Río, the predominant substrate comprises limestones, dolomites and marbles, which account for more than half of the municipality’s soils and provide a firm and reliable basis for foundations. The presence of fine sandstones and silts is limited, which significantly reduces the likelihood of problems caused by differential settlements. The high permeability attributed to the extensive aquifers ensures effective drainage, favouring high bearing capacities for most structures; however, the location of water masses must be considered, as they may alter conditions at certain sites.

Local seismicity in Palomares del Río is very low, with only a single recorded event over 30 years and a small maximum magnitude, so the seismic influence on structural design is practically negligible. There are no risks associated with karst or significant expansivity processes, since the contents of expansive clays are non-existent or dispersed in a non-clayey matrix, thereby ruling out possible volumetric instabilities. The main geotechnical factor that usually needs to be considered is the precise delimitation of the position of the water table level and the local characterisation of the limestone rock; these are key factors for a proper foundation geotechnical study.