Estudio geotécnico in Monforte del Cid

In Monforte del Cid, ground conditions are predominantly formed by sandstones, conglomerates and flysch formations, accompanied to a lesser extent by limestones, dolomites and marbles. This type of soil generally offers good bearing capacity for foundations, enabling direct solutions on competent substrata. However, the sporadic presence of fine sands and silts requires specific assessment, as these materials provide lower stability for supporting structures.

Local seismicity is very low, with only 5 events over 30 years and a maximum magnitude of 2, which implies a low seismic risk. However, the existence of karstic ground derived from limestones and dolomites makes it necessary to verify in detail the presence or activity of karst before carrying out any foundation work, as the associated voids and dissolution processes can compromise stability. In addition, the absence of clayey substrata eliminates the risk of shrink-swell (expansivity) in the area. The main technical consideration when carrying out a geotechnical study in the municipality is the possible impact of karst processes in the carbonate zones.