Estudio geotécnico in Segura de León

In Segura de León, the geological substrate is mainly dominated by slates and schists, followed in smaller proportions by granite, gneiss and other igneous rocks. These materials provide a competent and stable foundation for shallow and deep foundations, although the low permeability of these formations may limit the discharge of water and drainage capacity. In general, the bearing capacity of these soils is suitable for most building typologies, with it being advisable to locally assess the presence of alterations and fractured zones, which can influence ground behaviour.

Seismic activity in this municipality is practically non-existent, with a single minor event recorded in the last 30 years and a very low maximum magnitude, which makes it possible to rule out seismicity as a relevant constraint in projects. Although the non-clayey substrate eliminates the risk of expansivity, the possible presence of karst-related phenomena means that specific checks must be carried out before any foundation is executed, considering especially stability and the possibility of cavities at depth as the main factor for the geotechnical study.