Estudio geotécnico in Fuengirola

In Fuengirola, substrates are predominantly formed by slates and schists, accompanied to a lesser extent by sandstones, conglomerates and flysch. These materials generally provide adequate bearing capacity for conventional foundations and low permeability, although they may allow the existence of small superficial aquifers, especially in areas with sandstones and conglomerates. Layers with fine sands and silts, although infrequent, may require specific review to ensure they do not reduce load-bearing capacity, whereas outcrops of limestones, dolomites or granite are limited but also represent good points of support for the structure.

Seismic activity in Fuengirola is moderate, with 18 events over the last 30 years and a maximum magnitude of 4.4, which suggests the need for a basic seismic stability analysis but without any extraordinary requirements. There are no constraints associated with karst processes in the municipality, and the non-clayey substrate confirms the absence of risk due to expansivity. The key aspect for geotechnical studies in the area is the heterogeneity of the near-surface materials, which makes it essential to accurately characterise the stratigraphy during the borehole investigation campaign prior to any foundation work.