Estudio geotécnico in Ademuz

In Ademuz, soils are predominantly composed of sandstones, conglomerates and flysch, followed very closely by calcareous formations such as limestones, dolomites and marbles. These materials generally offer a good bearing capacity for direct foundations, although the formations may show variability in strength. The lower presence of gypsum, anhydrite and salts introduces a risk of dissolution processes that must be carefully assessed in field studies, as they may compromise ground stability under significant structural loads.

The municipality is located in an area of very low seismicity, with just 5 recorded events in the last three decades and a maximum magnitude of 2.7, which minimises the seismic influence on the design of foundations. Since the dominant substrate is not clayey, there is no risk of expansivity related to clay swelling. However, the existence of karst-related phenomena associated with limestones and dolomites underlines the importance of verifying possible voids and dissolution processes before proceeding with any type of foundation; the development of karstic cavities may constitute the main geotechnical constraint in Ademuz.