Estudio geotécnico in Guadassuar

The municipality of Guadassuar is characterised by a predominance of fine sands and silts, accompanied by a significant presence of limestones, dolomites and marbles, as well as compact gravels and sands. This lithological context, composed for the most part of medium-to-fine grained materials and calcareous soils, implies favourable bearing capacity for conventional construction projects, particularly over compact sand levels and calcareous formations. The minor presence of hard clays does not represent a significant constraint for the choice of foundation, whereas the generally low permeability supports stability, although possible shallow aquifers should be considered during excavation or drainage phases.

Seismicity in Guadassuar is classified as moderate, with 26 events over 30 years and a maximum recorded magnitude of 3.5, so seismic risk is low and does not constitute a critical limiting factor in structural design. It is important to note the presence of calcareous formations susceptible to karstification, which requires prior verification of the existence of voids or cavities before designing the foundations. The non-clayey substrate allows expansivity to be ruled out as a relevant geotechnical constraint. Thus, the main factor to consider in any geotechnical study in Guadassuar will be detailed inspection of karst potential, particularly beneath substantial buildings.