Estudio geotécnico in Chiloeches

In Chiloeches, the predominant geological substrate consists of limestones, dolomites and marbles, accompanied by a significant presence of sandstones, conglomerates and flysch. These materials, together with slates and, sporadically, compacted gravels and sands, generally provide a good bearing capacity for shallow or deep foundations, depending on the project. However, the high permeability associated with extensive aquifers can condition the design of the foundations, particularly in areas near bodies of water or where loose materials such as sands and gravels are present.

From a geotechnical point of view, Chiloeches is located in a high seismicity zone with more than 150 recorded events and a maximum magnitude (Mmax) of 4.6, which means it is essential to integrate seismic risk into the structural analysis. Likewise, the presence of carbonate formations makes it necessary to verify the existence of karst-related phenomena before designing the foundations, since they can seriously affect their stability and durability. The lack of clayey soils rules out expansive ground problems, so the main factors are seismicity and the possible karst processes in the subsurface.