Estudio geotécnico in Museros

In Museros, soils of fine sands and silts predominate, followed by significant areas of gravels and compact sands, which together make up the majority of the substratum. These granular materials usually exhibit good bearing capacity, thereby facilitating shallow foundation solutions provided that the degree of compaction is verified and that organic materials are absent at depth. Limestones and dolomites appear only in specific places and may locally influence geomechanical behaviour, as well as the ground’s permeability, given the frequently very permeable and productive nature of the aquifers present in the area.

Seismic activity in Museros is moderate, with 27 events in the last 30 years and a maximum magnitude (Mmax) of 3.4, which implies a low although not negligible seismic risk. The substratum, not being clayey, eliminates the risk of expansivity. However, the presence of carbonate formations suggests the possible existence of karstification; therefore, it is essential to check karst conditions before deciding the foundation type, this being the main geotechnical constraint for any urban or building development in the locality.