Estudio geotécnico in Gavarda

In Gavarda, the predominant soils are fine sands and silts, with a frequent presence of limestones, dolomites and marbles. This geological setting determines a moderate bearing capacity in alluvial areas, although the presence of carbonate rock provides good conditions for deep foundations when it occurs at shallow depth. The low permeability of the near-surface materials reduces the susceptibility to differential settlement, allowing safe support options for structures, although it is important to avoid areas close to bodies of water.

Seismicity in the municipality is very low, with only 6 recorded events over 30 years and a maximum magnitude of 2.9, so it does not constitute a relevant constraint for structural design. There are no risks associated with expansive soils, given that the subsoil is not clayey. However, particular attention must be paid to the possible presence of karst-related phenomena in the limestone and dolomite formations, so it is essential to carry out detailed checks of stability and continuity before executing any type of foundation, this being the main geotechnical consideration in the area.