Estudio geotécnico in Casserres

In Casserres, soils predominate that are formed by sandstones, conglomerates and flysch—materials that provide a stable geological base for most constructions. These strata generally exhibit an adequate bearing capacity, particularly in areas where the formations are compact and well cemented. However, given their low surface permeability, it is essential to assess the possible presence of aquifers at depth when designing foundations, as they could influence the ground’s behaviour in the long term.

The seismic activity recorded in Casserres is very low, with only 5 events over the last 30 years and low maximum magnitudes; as a result, its impact on structural design is residual. Although expansive clays occur in a subordinate form and are located in certain areas, their geotechnical influence is usually limited owing to the municipality’s climatic setting. The main constraint in the area lies in the correct characterisation of the local lithology and potential permeability variations with depth.