Estudio geotécnico in La Roda

In La Roda, the predominant substrate is formed by fine sands and silts, which implies moderate to good bearing capacity under normal conditions. The presence of soils with these characteristics requires a specific study to determine the suitability of the foundation, especially in buildings with significant loads. The relatively low permeability of the formations at depth, which may host aquifers of greater volume, is also a factor to be considered in order to avoid consolidation problems or differential movement.

The seismicity in La Roda is of low magnitude, with a maximum of 2.5 M and around 32 events over 30 years, so it does not represent a primary constraint in structural design. In addition, there are no signs of karst or risk of expansivity, ensuring greater ground stability. The absence of expansivity-prone soils means that swelling or shrinkage effects are unlikely in building projects in the area.