Estudio geotécnico in Mojados

In Mojados, compact gravels and sands predominate, forming its main geotechnical substrate and proving favourable for shallow foundations thanks to their adequate bearing capacity. Attention should be paid to the occasional presence of gypsum, anhydrite and salts, as these materials can induce dissolution processes in contact with water, affecting ground stability. Sandstone and conglomerate units are present in a secondary way, while masses of water, although less frequent, can locally influence saturation or increases in the groundwater table.

The seismicity in Mojados is classified as high, with more than 150 recorded events over 30 years and a maximum magnitude reaching 4.7, which implies that structural design must incorporate appropriate seismic criteria. In addition, the possible presence of karst requires prior verification before any foundation, to avoid differential settlements linked to dissolution processes. Although expansive clays appear in subordinate proportions and in climatically less active areas, it is recommended to confirm this on site. The main determinant for geotechnical studies in this municipality is the combination of seismic risk and the need to verify karst processes and associated dissolution linked to soluble materials.