Estudio geotécnico in Torremocha de Jarama

In Torremocha de Jarama, the predominant ground conditions mainly correspond to phyllites and schists, rocky materials that provide good bearing capacity for shallow and deep foundations owing to their cohesion and relative homogeneity. There is a significant proportion of groundwater bodies, which suggests high water table levels or soils that are temporarily saturated, whereas sandstones, conglomerates and even some carbonate outcrops (limestones, dolomites) appear to a lesser extent. The majority presence of low-permeability rocks may limit infiltration, although localised shallow aquifers can develop. This geological context influences the choice of foundation type, with careful analysis recommended in areas close to water bodies.

Seismic activity in the area is very limited, with only 5 recorded events over 30 years and a low maximum magnitude, which minimises the need to consider specific aspects of seismic risk for structural design. However, the presence, even if only localised, of carbonate materials advises checking for possible karst processes before proceeding with any foundation, as they could affect ground stability. No risks associated with expansivity are identified, since the subsoil is not clayey; therefore, the monitoring of possible karst cavities is the main geotechnical constraint in this municipality.