Estudio geotécnico in Higuera de la Sierra

In Higuera de la Sierra, the predominant geological substrate is made up of phyllites and schists, which provides soils with low permeability and generally stable behaviour. Less frequently, sandstones and conglomerates may occur, as well as specific bodies of granite. The bearing capacity is usually suitable for small- or medium-scale buildings, although the presence of superficial aquifers may affect moisture content and the condition of the foundations. It is essential to design the foundation according to the depth and continuity of the competent bedrock to ensure structural stability.

Seismicity in the area is very low, with only 4 recorded events in the last three decades and a low maximum magnitude of 2.1, so it does not represent a relevant constraint for construction. The substrate does not present any risk of expansivity as it is not clayey, ruling out pathologies associated with swelling. However, the possible presence of karstic formations requires verifying ground stability against voids or dissolution processes before carrying out any foundations; this is the main geotechnical constraint in Higuera de la Sierra.