Estudio geotécnico in Navalafuente

In Navalafuente, granito, gneiss and other igneous rocks predominate, covering approximately two thirds of the ground, followed by slates and schists in smaller proportions. These materials are characterised by high strength and low weathering susceptibility, which translates into excellent bearing capacity and a reliable direct foundation, although excavability may be moderately challenging due to the hardness of the substrate. The formations are generally impermeable, so the presence of water is mainly restricted to near-surface levels, with scant risk of the presence of compressible materials or soft soils.

Seismicity in Navalafuente is classified as very low, with only five recorded events over 30 years and a maximum magnitude of 3, which rules out the need to consider significant seismic effects in structural design. Since the substrate is not clayey, there are no risks associated with expansivity, and the absence of karst processes further simplifies the geotechnical analysis. The main limiting factor for the geotechnical study in the area will be the correct characterisation of the rock strata and their degree of weathering, both of which are essential to ensure ground stability and optimise the foundation.