Estudio geotécnico in Albox

In Albox, the dominant material in the subsurface corresponds to phyllites and schists, which implies moderate bearing capacity, with strata of fine sands and silts being common and possibly requiring special treatments if they are saturated. The occasional presence of limestones, dolomites and marbles introduces the possibility of locally higher mechanical competence levels, whereas compact gravels and sands are uncommon as a founding horizon. The substrate is characterised by low permeability, which may affect drainage in projects with basements or deep excavations.

Seismic activity in Albox is notable, with 51 events over 30 years and a maximum magnitude of 3.9, so it is relevant to take it into account in the overall ground assessment. In addition, the presence of carbonate materials indicates a risk of developing karst phenomena, so it is essential to check for the existence of cavities before defining the type of foundation. Since the substrate is not clayey, the risk of expansivity is ruled out, leaving the possible occurrence of karstification as the main factor to be analysed prior to the start of the works.