Estudio geotécnico in Almendral

In Almendral, sandstone, conglomerates and flysch predominate, accompanied by smaller proportions of overconsolidated clays and marls, igneous rocks such as granite and gneiss, as well as slates and schists. These materials generally offer high mechanical strength, which translates into a good bearing capacity for shallow and deep foundations. However, their low permeability can generate shallow groundwater levels, so it is essential to study this aspect during the geotechnical study.

Seismic activity in the area is very low, with only 3 events in the last 30 years and a maximum magnitude of 2.9, which minimises the influence of seismicity on structural design. The non-clayey substrate rules out the risk of expansiveness. It is essential to verify the presence of karst phenomena before designing any foundation, as they could affect ground stability and condition the choice of the most suitable foundation type.