Estudio geotécnico in Atzeneta d'Albaida

In Atzeneta d'Albaida, calcareous materials predominate, comprising essentially limestones, dolomites and marbles, which make up almost the entirety of the geological substrate. These formations are generally compact and provide a high bearing capacity, facilitating direct shallow surface foundations in most cases. The very limited presence of gravels and sands does not represent a relevant factor from a construction standpoint for this setting. The impermeable characteristics of the rocks may allow the development of localised superficial aquifers, although they do not significantly affect the overall bearing capacity.

Seismicity in the area is very low, given the small number of recorded events and a maximum magnitude that is negligible, which rules this out as a conditioning factor in structural design. Nevertheless, the nature of the substrate implies the possible existence of karstic cavities; therefore, it is essential to thoroughly verify the presence of karstification phenomena before proceeding with any foundation. As it is a non-clayey substrate, the risk of expansive soils is ruled out; thus, the main technical consideration lies in detecting and assessing the risk associated with karst.