Estudio geotécnico in Peal de Becerro

In Peal de Becerro, soils formed by limestones, dolomites and marbles predominate, representing the largest part of the local geological substratum. These materials, generally compact in nature, offer good conditions for bearing capacity for conventional foundations, although the point-like presence of sandstones and conglomerates is also relevant in specific areas. The low overall permeability of the ground may facilitate stability with respect to water movements, although shallow aquifers may exist in certain zones that must be verified during the geotechnical study.

As regards seismicity, a high number of events is recorded (171 in the last 30 years), although the maximum magnitude observed (Mmax 4.4) does not reach the most demanding structural thresholds. It is essential to note the potential presence of karstic phenomena in the area, associated with the calcareous materials, which makes it necessary to check stability against voids and dissolution before defining the foundation. Given the non-clayey substratum, the risk of expansiveness is ruled out. The main constraint for the geotechnical study in Peal de Becerro will be verification of the karst and a detailed assessment of local conditions in order to guarantee the safety of the foundations.