Estudio geotécnico in Estivella

In Estivella, the subsurface is dominated mainly by limestones, dolomites and marbles, which account for more than 44% of the materials encountered, followed by sandstones and conglomerates, as well as certain occurrences of gravel and compacted sands. This lithological context generally provides a high bearing capacity and good stability for the construction of shallow foundations, although the frequent presence of extensive, highly permeable aquifers may require special care in controlling the groundwater level, particularly in areas where less consolidated gravels and sands are found.

Seismic activity in Estivella is moderate, with 27 recorded events over the last 30 years and a maximum magnitude of 3.4, which implies routine seismic monitoring but without demanding structural constraints. The existence of karstification in the calcareous formations requires prior verification of cavities or dissolution before carrying out any foundation, as these phenomena can compromise ground stability. The absence of an argillaceous substrate eliminates the risk of expansivity, the main constraint being the possible presence of karst processes that must be investigated in detail in each geotechnical study.