Estudio geotécnico in El Paso

In El Paso, formations of sandstone, conglomerates and flysch predominate; these materials occur in the substrate in the great majority. These lithologies usually give the ground an adequate bearing capacity for most buildings, although the presence of bedding stratification and low permeability are factors to take into account when designing the foundations. Aquifers may be found at some depth, so it is important to consider the possible variation in the groundwater table level when planning the support for strip footings or rafts.

Seismic activity in the area is moderate, with 11 events recorded over the last 30 years and a maximum magnitude of 2.2, which implies a low seismic risk for construction projects. Since the substrate is clearly non-clayey, risks associated with expansive soils are ruled out. The main determining factor in El Paso is the nature of the flysch and the need to verify the stability and homogeneity of these materials at depth during the geotechnical study.