Estudio geotécnico in Santa Olalla del Cala

In Santa Olalla del Cala, the predominant geotechnical substrate is formed by slates and schists, representing close to 59% of the soils, followed by granite, gneiss and other igneous rocks, as well as some reduced bands of sandstones and conglomerates. These lithologies give the ground high strength and low deformability, which promotes stability and provides good bearing capacity for shallow and semi-deep foundations. However, the predominant presence of low-permeability materials may favour the local accumulation of surface water, which requires considering suitable drainage in building projects.

Seismic activity in the municipality is significant, with 106 recorded events over 30 years, although with relatively low magnitudes (Mmax 2), which reduces its influence on structural design. However, the possible presence of karstification makes it necessary to carry out specific checks before carrying out any foundation work, since cavities or dissolutions at depth could represent a significant geotechnical risk. The non-clayey substrate eliminates concern about expansivity-related phenomena, so verification of the possible karst is considered the geotechnical factor that may most affect foundation work in the area.