Estudio geotécnico in Torremolinos

In Torremolinos, geotechnical studies usually find soils dominated by slates and schists, metamorphic materials that provide a good foundation substrate in most cases. In addition, fine sands and silts appear, as well as levels of gravels and compacted sands in smaller proportions, which can offer medium to high bearing capacities when sufficiently densified. The occasional presence of limestones, dolomites and marbles implies the possibility of encountering stiffer zones, although attention must be paid to the continuity and alteration of these formations. With regard to permeability, it is worth highlighting the existence of discontinuous aquifers with variable behaviour, which may affect drainage and the stability of excavations.

The municipality exhibits moderate seismicity, with 26 events over the last 30 years and a maximum magnitude of 3.3, placing it within parameters that do not significantly condition the structural calculation of typical buildings. However, due to the presence of carbonate formations such as limestones and dolomites, it is essential to check for the possible presence of karst cavities before defining any foundation solution, to avoid unexpected settlements. The dominant subsoil is not clayey, so the risk of expansivity is ruled out. Thus, the main precaution in Torremolinos is the detailed characterisation of the karst and its influence on the stability of the foundation ground.