Estudio geotécnico in Anglesola

In Anglesola, the dominant geological substrate is composed mainly of compacted gravels and sands, which account for 87.5% of the total, occasionally accompanied by sandstones, conglomerates and flysch. These materials provide high and homogeneous bearing capacity, which favours options for direct foundation, although the localised presence of shallow aquifers due to the relatively impermeable nature of the formations must be verified in advance to ensure stability and the correct management of groundwater on site.

Seismicity in Anglesola is very low, as shown by just three recorded events over the last 30 years and a maximum magnitude of 2.5, which minimises the influence of this factor on structural design. Although subordinate expansive clays or in climatic zones without any notable water input exist, the risk associated with expansivity is low in most of the municipality due to the limited presence of this type of soil and environmental conditions. The main geotechnical limiting factor therefore lies in the detection and accurate characterisation of those specific areas where clay formations may be present prior to foundation.