Geotechnical study in Trasmiras
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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 localities of Trasmiras.
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 Trasmiras whenever it suits you, agreeing on a day and time.
Types of ground in Trasmiras
In Trasmiras, sandstone, conglomerates and flysch predominate as the substrate, accompanied in smaller proportions by slates, schists, as well as by clays and hard marls. These materials generally exhibit good mechanical behaviour, offering medium to high bearing capacities, which facilitates the design of shallow foundations for light and medium-sized buildings. However, the occasional presence of deltaic muds and peats requires precise location to prevent their use as a bearing stratum, as they may compromise the stability of the foundation.
Seismic activity in Trasmiras is moderate, with a record of 11 events over thirty years, but the low maximum magnitude (Mmax 2.8) implies a reduced seismic risk for structural design. Since the substrate is mostly non-clayey, the risk of expansivity is ruled out, which constitutes a significant advantage in the development of projects. The main geotechnical constraint in the area is the identification and avoidance of soft layers of mud or peat, ensuring a safe foundation on the predominant 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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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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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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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 Trasmiras
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 ... |
| Phyllites and schists | None | Media | Media | Media | Shallow foundation if the stratum is competent. Strong b... |
| Overconsolidated clays and marls (Duras) | Media | Media | Downward | Downward | Direct foundation is viable. Piling is rarely resorted t... |
| 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 · Trasmiras
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 Trasmiras · Based on GEODE soil types
Indicative profile based on GEODE soil types and typical CTE thicknesses
Seismic risk in Trasmiras
- 1 M 2.8 2010
- 2 M 2.8 2025
- 3 M 2.2 2018
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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