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MASW Seismic Survey & VS30 Classification West Valley City

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West Valley City grew fast. Orchards and farmland flipped to subdivisions and tilt-up commercial in two generations. That pace left gaps in the geotechnical record. A lot of the subsurface here is Lake Bonneville sediment, but the stiffness varies block by block. The 2020 Magna quake reminded everyone that the Wasatch Fault is active. Our MASW survey fills the data gap. It gives the structural engineer a measured VS30 value and an IBC site class, not an assumed one. That number changes foundation design, seismic base shear, and whether you need a liquefaction assessment before the footing is drawn. We run the survey, process the dispersion curve, and deliver the shear wave velocity profile in four business days.

A measured VS30 in West Valley City often drops the site class one letter compared to the default code assumption — and that changes the seismic design category.

Process and scope

The soil difference between Hunter and Granger is night and day. Hunter sits on stiffer Pleistocene gravels. Granger has deeper fine-grained deposits with lower shear wave velocity. A site class C in Hunter might be a D or E in Granger. That is a real cost driver. We deploy a 24-channel seismograph with 4.5 Hz geophones and an active sledgehammer source. The array captures Rayleigh wave propagation down to 30 meters. Inversion yields a 1D shear wave velocity profile. The VS30 is calculated per IBC 2021 criteria. Where the near-surface is uncertain, we pair MASW with a CPT test to ground-truth the stratigraphy. The output goes straight into the structural model.
MASW Seismic Survey & VS30 Classification West Valley City
Technical reference image — West Valley City

Local geotechnical context

We use a Geometrics Geode seismograph with a spread of two dozen geophones. The array is 69 meters long for a 30-meter target depth. On a West Valley City commercial lot, we lay the line parallel to the proposed building footprint. No drilling, no cuttings, no traffic disruption. The hammer hits a steel plate, the geophones catch the Rayleigh wave, and the software stacks the shots. The risk in skipping this survey is a site class assumption that does not hold. Default site class D is common in the IBC, but a stiff profile in Hunter might qualify as C. That reduces base shear and saves steel. The opposite is worse: assuming C and discovering soft clay at 12 meters during excavation. Then the foundation is locked, and the structural engineer has to retrofit the lateral system.

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Email: info@geotechnicalengineering.sbs

Technical parameters

ParameterTypical value
MethodActive MASW, linear array, sledgehammer source
Geophone24-channel, 4.5 Hz vertical component
Depth of investigation30 m (100 ft) standard, deeper on request
Key outputVS30 (m/s), IBC Site Class A through E
Data processingDispersion curve extraction, 1D shear wave velocity inversion
Reporting standardASCE 7-22 Section 20, IBC 2021 Chapter 16
Typical turnaround4 business days, field-to-report

Other technical services

01

VS30 Site Classification

Full IBC site class letter delivered with the shear wave velocity profile. We provide the 30-meter average and the interval velocities in a signed report ready for permit submittal.

02

Combined MASW + Geotechnical Drilling

We run the seismic line and a mud rotary boring on the same day. The driller logs the stratigraphy while the geophone array records the Rayleigh wave. You get a unified ground model.

03

Site-Specific Seismic Hazard Analysis

For Risk Category III and IV structures, we pair the VS30 profile with a probabilistic seismic hazard assessment. The output is a design response spectrum per ASCE 7 Chapter 21.

Applicable standards

ASCE 7-22 Minimum Design Loads — Site Classification Procedure, IBC 2021 Section 1613 — Site Class Definitions and VS30, ASTM D7400 — Standard Test Methods for Downhole Seismic Testing (referenced for methodology)

Common questions

What is the cost of a MASW survey in West Valley City?

A standard active MASW survey with one array and VS30 classification runs US$1,860 to US$3,200 depending on site access, array length, and whether we combine it with a boring. The price includes field work, dispersion analysis, inversion, and the signed report.

How does MASW determine the IBC site class?

The array records Rayleigh wave propagation. We extract the dispersion curve, invert it to a shear wave velocity profile, and compute the average VS30 in meters per second. That value maps directly to Site Class A, B, C, D, or E per IBC Table 1613.2.3.

Can you run the survey on a paved lot in West Valley City?

Yes. We use bolt-down geophones on asphalt or concrete. The sledgehammer source works on pavement. The data quality is often better than on soil because the coupling is cleaner. We do not core or cut the surface.

What is the difference between active and passive MASW?

Active MASW uses a sledgehammer or weight drop and reaches 25 to 40 meters. Passive MASW uses ambient noise and goes deeper, up to 100 meters. For IBC site classification, active is standard. We add passive only when the structural engineer needs a deeper profile for basin effects or site response modeling.

Location and service area

We serve projects in West Valley City and surrounding areas.

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