Estudio geotécnico in Montemolín

In Montemolín, the geological substrate is formed mainly by slates and schists, accompanied in smaller proportions by granite, gneiss and other igneous rocks, as well as sandstones and conglomerates. These materials are characteristically compact and have low permeability, which limits the presence of deep aquifers and provides ground stability. Since they are hard soils with little weathering, bearing capacity is usually good, allowing shallow, direct-type foundations in many areas, although the possible presence of localised alterations must always be checked.

Seismicity in the area is notable, with 61 events recorded over the last 30 years, although with a low maximum magnitude (Mmax 3.1), so that seismic risk, while not critical, must be assessed in the geotechnical study. On the other hand, although the substrate does not present a risk of expansiveness because it is not made up of clayey materials, there is the possibility of karstification in the surrounding area; thus, it is recommended to thoroughly verify the absence of voids and subsidence before undertaking any foundation, this being the main geotechnical factor to control in Montemolín.