GEOTECHNICAL ENGINEERING
BELFAST
HomeGeophysicsSeismic tomography (refraction/reflection)

Seismic Tomography Surveys (Refraction & Reflection) in Belfast

Sound ground. Sound decisions.

LEARN MORE

The geophone array stretches across the site in a carefully surveyed line, each sensor spiked firmly into the Belfast clay. A sledgehammer strikes the steel plate at the shot point and the seismic pulse races downward, refracting off the sandstone bedrock and reflecting from the clay-till interface. This is seismic tomography in practice—a technique that builds a continuous image of the subsurface from dozens of individual wave paths. In Belfast, where the glacial history has left a chaotic sequence of stiff till, soft clay, and weathered rock, the method reveals the hidden architecture that boreholes alone can miss. The equipment is portable enough to deploy on confined urban plots near the Lagan riverfront, and the data density is high enough to map subtle velocity variations across the 280,000-square-metre footprint of a typical city-centre redevelopment. When combined with targeted SPT drilling for point calibration, the resulting velocity model gives engineers a solid basis for designing foundations that work with the ground rather than against it.

A single seismic line across the Lagan Valley can map bedrock depth, identify buried channels, and deliver the Vs30 profile needed for seismic design—all in one working day.

Our service areas

How we work

BS 5930:2015 and BS EN 1997-2 (Eurocode 7 Part 2) set the framework for ground investigation in the UK, and in Belfast their guidance on geophysical methods carries particular weight. The city straddles the boundary between the Antrim basalts to the north and the Triassic sandstones and Mercia Mudstone beneath the Lagan Valley, with up to 40 metres of glacially disturbed overburden in between. Seismic refraction tomography maps the top-of-bedrock profile and identifies low-velocity zones that correspond to soft alluvial pockets along the buried course of the Blackstaff River. Reflection profiling, meanwhile, resolves deeper stratigraphy where the velocity contrast between the Mercia Mudstone and the underlying Sherwood Sandstone is sharp enough to produce a clear reflector.
  • Refraction tomography for bedrock depth and rippability assessment on brownfield sites.
  • Reflection profiling for basin geometry and deep fault detection beneath proposed high-rise structures.
  • Surface-wave analysis (MASW) integrated into the same spread for shear-wave velocity profiles to 30 metres.
In the Titanic Quarter, where fill thickness varies unpredictably over the former shipyard, MASW surveys paired with refraction lines have become the standard approach for mapping Vs30 without the access constraints of borehole methods. The data feeds directly into seismic site classification under BS EN 1998-1 and the UK National Annex, producing the ground-type profiles that structural engineers need for Eurocode 8 compliance.
Seismic Tomography Surveys (Refraction & Reflection) in Belfast
Technical reference — Belfast

Local ground factors

Belfast’s industrial expansion in the 19th and early 20th centuries reshaped the city’s ground surface as dramatically as any geological process. The Lagan riverfront was progressively reclaimed with a mixture of dredged silt, foundry waste, and demolition rubble, creating a zone of made ground that now underlies some of the city’s most valuable development land. Victorian-era maps show the original shoreline running through what is now the Cathedral Quarter, and the buried dock infrastructure—timber piles, masonry walls, filled basins—remains in place beneath the modern streets. Seismic tomography can miss thin void spaces or isolated timber obstructions, and its resolution degrades where the velocity contrast between made ground and natural soils is minimal. The hazard lies in assuming that a clean velocity profile means clean ground; local experience shows that supplementary intrusive investigation is essential wherever the historical record indicates former industrial use. The risk is not theoretical—projects at the Gasworks site and the Sirocco Quays have encountered unexpected buried structures that delayed foundation works by weeks. A seismic survey that integrates historical land-use mapping with targeted verification boreholes provides the most reliable path to reducing this uncertainty.

Need a geotechnical assessment?

Reply within 24h.

Email: contact@geotechnical-engineering.biz

Relevant standards

BS 5930:2015 – Code of practice for ground investigations, BS EN 1997-2:2007 – Eurocode 7: Geotechnical design – Ground investigation and testing, BS EN 1998-1:2004 + UK National Annex – Eurocode 8: Seismic design, BS 1377 – Standard Guide for Using the Seismic Refraction Method

Typical values

ParameterTypical value
MethodSeismic refraction & reflection tomography
Typical survey depth (refraction)5–80 m (depending on spread length)
Typical survey depth (reflection)20–500+ m
Source typeSledgehammer, weight drop, or seismic gun
Receiver spacing1–5 m (refraction), 2–10 m (reflection)
OutputP-wave velocity sections, bedrock profiles, Vs30 maps
Compliance standardBS 5930:2015, BS EN 1997-2:2007, BS EN 1998-1

Frequently asked questions

How much does a seismic tomography survey cost in Belfast?

For a typical refraction tomography survey on a Belfast site—say a single 115-metre line with 24 geophones and sledgehammer source—the cost generally falls between £2,460 and £4,200. The final figure depends on line length, number of shots, access conditions (city-centre traffic management adds cost), and whether reflection or MASW processing is included. We provide a fixed-price quotation after reviewing the site location and your specific investigation objectives.

What depth can seismic refraction and reflection surveys reach in Belfast's ground conditions?

Refraction tomography typically reaches 15 to 40 metres depth in Belfast, depending on the spread length deployed; a 115-metre spread with hammer source will reliably image to about 25–30 metres. Reflection profiling can reach 200 metres or more in the Lagan Valley where the Sherwood Sandstone provides a strong acoustic impedance contrast. Maximum depth is always site-specific and depends on the velocity structure and source energy.

Do you need road closures or traffic management for seismic surveys in Belfast?

For surveys on private land or construction sites, no traffic management is needed. For surveys on public roads or footpaths within Belfast city centre, we coordinate with the Department for Infrastructure (DfI) Roads to obtain the necessary permits and arrange temporary traffic management. We handle the entire process—from permit application to traffic light setup—so your project stays on schedule.

How does seismic tomography compare with boreholes for site investigation?

They complement each other rather than compete. Boreholes provide direct samples and point-specific strength data, but the information between boreholes is always an interpolation. Seismic tomography provides continuous coverage between measurement points, revealing lateral variations that boreholes spaced 20 metres apart can miss. In Belfast’s complex glacial deposits, the most reliable ground model comes from calibrating seismic velocity sections with borehole logs and, where available, CPT soundings that provide a continuous vertical profile at a specific location.

Location and service area

We serve projects across Belfast and surrounding areas.

View larger map