Geotechnical study in Xinzo de Limia
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Comprehensive Geotechnical Studies
We combine field analysis and laboratory testing to provide accurate technical reports and foundation solutions.
Expert professional
Technicians with more than 15 years of experience in the industry. We are specialists in access to difficult locations such as sites with level changes, basements, etc.
Accredited
Geotechnical calculations comply with the rules established by Eurocode 7, UNE-EN ISO 22476-4:2016.
Best price
Very competitive prices. The best prices for geotechnical studies in Spain. Request a quote and check it.
Speed and quality
Within 7 to 10 days you will receive a signed report from a geologist. It is mandatory in order to carry out new construction or refurbishment works that involve modifications to the structure.
Work areas
We provide Geotechnical study in all locations of Xinzo de Limia.
This includes the following geographical areas: Province of A Coruña, Lugo Province, Province of Ourense, Province of Pontevedra, Galicia and surrounding areas.
We come to your home in Xinzo de Limia whenever it suits you, agreeing a day and time.
Types of ground in Xinzo de Limia
In Xinzo de Limia, formations of sandstones, conglomerates and flysch predominate, accompanied by smaller levels of overconsolidated clays and marls, as well as slates and schists. These materials typically provide good to moderate bearing capacity, especially in areas where hard, compact materials prevail. However, the occasional presence of muds and peats of deltaic origin requires special attention, as these soils are not suitable as a supporting layer for foundations and must be avoided or treated if encountered within the project site.
Seismicity in the municipality is considered moderate, with 36 recorded events in the last 30 years and a maximum magnitude of 3.7, which implies the need for a basic analysis of seismic stability in the design, although without special structural requirements. The non-clayey substratum rules out significant expansivity risks and there are no constraints associated with karst processes. The main aspect to be verified in a geotechnical study will be the detection and treatment of soft soils of mud or peat type, always prioritising foundation solutions over the dominant hard strata.
Sandstones, Conglomerates and Flysch
Sedimentary rocks formed by the cementation of fragments of other pre-existing rocks. They include sandstones (cemented sand), conglomerates (cemented gravels) and the rhythmic alternation of sandston
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Overconsolidated clays and marls (Duras)
Cohesive soils with a hard feel, sometimes with a rock-like appearance when dry (grey marls, pre-Pyrenean facies, deep Guadalquivir basin). They have a long history of geological compression in the pa
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Phyllites and schists
Metamorphic rocks characterised by their foliation (parallel planes of weakness or slaty cleavage). Very common in Galicia, Asturias, the north of León, Extremadura and Sierra Morena. They are highly
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Fangy clays and peats (Deltaic)
Soils from the Holocene period, unconsolidated, flowing muds, black in colour with a very strong organic component, sometimes in the form of pure rotting vegetable matter (peat bogs). The mud compress
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Fine sands and silts
Fine to very fine granular soils with medium to loose compacity. Typical of floodplains and coastlines. Although they can support light buildings, they are treacherous soils linked to water processes:
View detailsConstruction risks in Xinzo de Limia
Approximate estimates. They do not replace the geotechnical study.
| Soil type | Expansivity | Settlements | Water table | Seismicity | Minimum foundation |
|---|---|---|---|---|---|
| Sandstones, Conglomerates and Flysch | None | Media | Media | Media | Direct foundation is feasible in most cases. For flysch ... |
| Overconsolidated clays and marls (Duras) | Media | Media | Downward | Downward | Direct foundation is viable. Piling is rarely resorted t... |
| Phyllites and schists | None | Media | Media | Media | Shallow foundation if the stratum is competent. Strong b... |
| Fangy clays and peats (Deltaic) | Downward | High | High | High | Inviable with any natural means. Drive tests of enormous... |
| Fine sands and silts | None | High | High | High | To avoid local punching, the foundation slab is used ext... |
Interactive geological map · Xinzo de Limia
Mapping: IGME GEODE 50k · IGME MAGNA 50 · ICGC (Catalonia)
Geological Viewer
IGME · ICGC- Click on the map to see the geology at the point.
- Use the layer buttons to switch between geological views (GEODE, MAGNA, Lithology, Hydrogeology).
- Adjust the opacity of the geological layer with the control below.
- Press the full-screen button to expand the viewer.
Geological information
Typical stratigraphic profile
Indicative subsurface cross-section in Xinzo de Limia · Based on GEODE soil types
Indicative profile based on GEODE soil types and typical CTE thicknesses
Seismic risk in Xinzo de Limia
- 1 M 3.7 2000
- 2 M 3.3 2021
- 3 M 2.8 2010
How do we carry out your geotechnical study?
Step
Free quote
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Step
We arrange a day
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Step
Conducting the geotechnical study
We’re going to move and carry out the study. In an hour or two we’ll have finished.
Step
Report submission
Within a week we will send you the signed documents of the geotechnical study by an accredited geologist.
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