Estudio geotécnico in Valdetorres de Jarama

In Valdetorres de Jarama, masses of water and sedimentary formations such as sandstones, conglomerates and flysch predominate, accompanied in smaller proportions by shales and schists. These soils generally provide an acceptable bearing capacity for conventional foundations, although the presence of discontinuous aquifers implies the need to assess possible changes in hydrogeological conditions and carry out detailed studies to determine optimal support depths and avoid differential settlement.

Seismicity in the area is very low, with only 5 recorded events over 30 years and a maximum magnitude of 3, which means it does not constitute a relevant constraint for structural design. Although the possible presence of non-expansive or dispersive clays is indicated, the risk of expansivity must be assessed on a case-by-case basis, as it could affect the stability of shallow foundations. In this context, localised expansivity is the main geotechnical consideration for projects in this municipality.