Estudio geotécnico in Godelleta

In the municipal district of Godelleta, carbonate materials predominate, such as limestones, dolomites and occasionally marbles, which provides a generally competent substrate with high bearing capacity for foundations. Fine sands and silts, although present to a lesser extent, may be suitable for supporting structures provided that their compactness is verified. Hard clays and marls occur only in isolated areas, and in general do not represent a major constraint. The notable permeability of the substrate, derived from the nature of the extensive aquifers, has a positive influence on drainage and reduces the problems associated with the accumulation of water beneath foundations.

Seismicity in Godelleta is moderate, with 10 events in the last 30 years and a maximum magnitude below 3, which minimises the relevance of seismic action in structural design. It is important to emphasise that the extensive presence of carbonate materials increases the likelihood of karst-related phenomena; therefore, any possible cavities or dissolution features must be rigorously checked before carrying out any foundation. Since the dominant substrate is not clayey, the risk of expansiveness is ruled out as a relevant constraint in the area.