Geotechnical study in Xunqueira de Ambía
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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 towns and cities of Xunqueira de Ambía.
This includes the following geographical areas: Province of A Coruña, Lugo Province, Province of Ourense, Province of Pontevedra, Galicia and the surrounding areas.
We go to your home in Xunqueira de Ambía when it suits you, arranging a day and time.
Types of ground in Xunqueira de Ambía
In Xunqueira de Ambía, the predominant substrate consists of sandstones, conglomerates and flysch, representing most of the materials in the municipality. In general, these ground conditions provide good bearing capacity conditions for shallow foundations, although it will be necessary to analyse any occasional levels of clays and hard marls which, although overconsolidated, may have variable behaviour depending on their moisture condition or fracturing. It is important to take particular care regarding the local presence of muds and peats of deltaic origin, which are not suitable for supporting foundations due to their low strength and high compressibility, and should therefore be avoided as a structural bearing stratum.
Seismicity in this area is moderate, with 18 recorded events in the last 30 years and a maximum magnitude of 3.1, which indicates that seismic risk is low from a structural point of view and does not significantly condition the design. There are no signs of karstification or problems associated with gypsum, salts or anhydrites. In addition, the absence of a clayey substratum excludes the risk of expansivity, simplifying the predictability of geotechnical behaviour. Therefore, the main local geotechnical constraint lies in identifying and avoiding foundation settlement on muds or peats, prioritising outcrops of hard, competent materials.
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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Water mass
Area corresponding to rivers, lakes, reservoirs, lagoons, permanent marshes or submerged coastal strips. The point consulted lies on a body of water identified cartographically by the IGME in its geol
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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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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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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 Xunqueira de Ambía
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... |
| Water mass | None | Downward | High | Downward | It is not possible to found on a body of water. If the p... |
| Fangy clays and peats (Deltaic) | Downward | High | High | High | Inviable with any natural means. Drive tests of enormous... |
| Phyllites and schists | None | Media | Media | Media | Shallow foundation if the stratum is competent. Strong b... |
| Fine sands and silts | None | High | High | High | To avoid local punching, the foundation slab is used ext... |
Interactive geological map · Xunqueira de Ambía
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 Xunqueira de Ambía · Based on GEODE soil types
Indicative profile based on GEODE soil types and typical CTE thicknesses
Seismic risk in Xunqueira de Ambía
- 1 M 3.1 2006
- 2 M 3 2007
- 3 M 2.9 2016
How do we carry out your geotechnical study?
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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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