Estudio geotécnico in Albalate de Cinca

In Albalate de Cinca, soils formed by sandstones, conglomerates and flysch predominate, making up more than 70% of the substrate. These materials generally exhibit an adequate bearing capacity for shallow foundations, although it is essential to assess the possible local presence of fine sand and silt layers, which are distinguished by their lower cohesion. In specific areas, deposits of compact gravels and sands may also be found, which are favourable for construction, although it is always recommended to ensure the regularity of the bearing layers by means of an in-depth geotechnical study.

Seismicity in Albalate de Cinca is considered high, with more than 150 events over 30 years and a maximum magnitude (Mmax) of 4.8, which requires incorporating earthquake-resistant criteria in the structural design of buildings. No concerns have been identified regarding karst or significant expansivity, as expansive clays occur in a subordinate way or in climatic contexts that minimise their influence; thus, the main constraint for the project will be the high seismicity, which must be assessed together with the characterisation of the bearing capacity of the detrital materials present.