Estudio geotécnico in Cervantes

In Cervantes, soils are predominantly composed of phyllites and schists, materials with high density and low permeability. These lithologies generally offer notable stability for shallow foundations, although it is common for there to be altered near-surface layers that may need to be removed or treated before structural support. The low permeability limits infiltration, which benefits the geotechnical performance in relation to problems of differential settlement over time and enables an adequate bearing capacity, except in areas with intense weathering.

With regard to seismicity, Cervantes exhibits moderate activity with 24 events over 30 years and a maximum magnitude of 4; therefore, although limited, the seismic action should be taken into account in structural design when dealing with sensitive buildings. The non-clayey nature of the ground rules out risks associated with expansive soils. It is important to highlight the possibility of karst-related processes; therefore, it is recommended to thoroughly verify the presence of cavities or dissolution beneath the foundation area to ensure the safety and durability of the structures.