Estudio geotécnico in La Orotava

In La Orotava, the geological substrate is predominantly composed of sandstones, conglomerates and flysch, which provides competent support for foundations, with good bearing capacity. Due to the permeable nature of these soils and the presence of perched aquifers or aquifers associated with contacts between formations, special attention is required for the drainage and control of groundwater during construction, although generally they do not limit the usual types of shallow or deep foundations.

Seismic activity in this area is moderate, with 11 recorded events over thirty years and a low maximum magnitude of 2.2, so the seismic risk is limited and does not represent a significant constraint for structural design. As no karst risk has been detected and there is no presence of expansive clays, the main geotechnical constraint in La Orotava lies in the management of groundwater and the correct characterisation of the groundwater table during the geotechnical study.