Estudio geotécnico in Segurilla

In Segurilla, the predominant subsoil is made up mainly of granite, gneiss and other igneous rocks, accounting for more than 90% of the ground, with a very limited presence of limestones, dolomites, marbles and slates. This type of rock formation is usually highly competent from a geotechnical point of view, offering high bearing capacities and allowing the execution of shallow (direct) foundations in most cases. In addition, the generally low permeability limits the presence of any significant groundwater, although small superficial aquifers may exist associated with local fracturing of the bedrock mass.

As regards seismicity, Segurilla shows high activity, with more than 200 recorded events over 30 years and a maximum magnitude of 5.1, so it is essential to consider seismic actions in the structural design of any building. Since the subsoil is not clayey, the risk of ground expansiveness is ruled out. The main limiting factor in this locality lies in the need for a detailed seismic study and the appropriate characterisation of the bedrock mass to ensure the stability and safety of the foundations.