Estudio geotécnico in Montefrío

In Montefrío, the geological substrate is dominated by limestones, dolomites and marbles, high-competence materials with good bearing capacity, which generally allows for direct, shallow foundations. Although fine sands, silts, sandstones and conglomerates are also present in a secondary way, their distribution is more specific and they rarely significantly influence the choice of foundation. The low presence of clays and hard marls reduces the risk of differential settlement consolidation, but the possible occurrence of shallow aquifers means that water control on site must be considered.

Local seismicity is moderate, with 19 recorded events over 30 years and a maximum magnitude of 3.5, which implies a limited seismic risk in structural design. However, the existence of karst formations associated with the limestones and dolomites requires specific verification of cavities or conduits before defining the foundation solution, this being the main geotechnical constraint in the area. The non-clayey substrate rules out problems of ground expansiveness.