Estudio geotécnico in Poble Nou de Benitatxell, the/Benitachell

The dominant substrate in Poble Nou de Benitatxell is composed mainly of limestones, dolomites and marbles, which form a soil with high strength and good bearing capacity. This geological character often favours direct foundations, provided that account is taken of the depth of the water table and the presence of faults or fractures in the rock, since the permeability of the aquifers can influence the stability of structures.

The seismicity in the area shows moderate activity, with 52 events over 30 years and an Mmax of 3.4, which implies a low seismic risk that should be considered in structural design. The absence of karst and the lack of expansivity in the soils make it possible to reduce geotechnical constraints, although high permeability may require additional monitoring in the study of groundwater levels and stability against possible earthworks movements.