Estudio geotécnico in Tornesa, la

In La Pobla Tornesa, the predominant geological substrate is composed of slates and schists, materials that are very frequently present in the area. This type of soil generally exhibits low permeability, although there are shallow aquifers at certain points of higher elevation. The bearing capacity is usually suitable for buildings, although foliation and possible local weathering may influence the selection and depth of the foundation; therefore, a detailed characterisation is recommended during the geotechnical study phase.

With regard to seismicity, La Pobla Tornesa shows high seismic activity, with approximately 200 events in the last 30 years and a maximum magnitude of 4.7, which makes it necessary to consider the seismic requirements in the structural design of new buildings. Although expansive clays appear in a subordinate manner or in localised areas, these are usually associated with climatic conditions in which the development of expansivity is attenuated; nevertheless, their specific control should not be ruled out. In conclusion, seismicity constitutes the main technical constraint, requiring a detailed approach during the geotechnical study phase.