Naas has a history that runs deeper than the M7 motorway that bypasses it. The town grew around a Norman settlement, but its underlying geology tells a much older story of glacial deposition and weathered limestone. This patchwork of stiff till, soft alluvial pockets, and occasional karst features creates a variable geotechnical profile that demands attention when designing for seismic loads. While Ireland sits away from active plate boundaries, the National Annex to Eurocode 8 assigns a low-to-moderate seismic hazard. A standard site class from a desk study is not enough. We run the MASW survey right through the site to measure Vs30 directly, because generic bedrock maps miss the localized drift deposits that can amplify ground motion in Naas. Our seismic microzonation approach builds a site response model from field data, not assumptions, letting structural engineers justify their design spectra with confidence and meet the requirements of I.S. EN 1998-1:2005 for each plot.
Ireland's low seismicity does not mean zero risk—local soft ground can amplify long-period motion by a factor of two or more, and only site-specific measurement catches it.
Service characteristics in Naas

Risks and considerations in Naas
The Irish midlands are not known for dramatic seismic events, but the contrast between the dry limestone uplands east of Naas and the low-lying floodplain along the canal creates a distinct geotechnical risk: basin-edge effects. Seismic waves entering the softer basin sediments can get trapped and amplified, producing longer shaking duration than the bedrock reference motion would predict. This matters for industrial buildings with long fundamental periods and for multi-story residential blocks now common on the Naas outskirts. Skipping a site-specific seismic microzonation study leaves the structural analysis blind to these local amplification patterns. We also check for cyclic softening in the glacial lake clays—soils that look stable under static load but can lose stiffness rapidly under repeated shear strain. The Eurocode 8 framework encourages such detailed investigation for importance class II and III structures, and our laboratory, accredited to ISO 17025, runs the full suite of dynamic tests to feed a defensible one-dimensional or two-dimensional ground response model.
Our services
We deliver seismic microzonation as a complete package—from initial field survey through to the final design spectrum. The work folds into the wider geotechnical investigation for your Naas project, saving time and ensuring consistency between the ground model and the seismic parameters.
Site-Specific Seismic Hazard Assessment
Geophysical survey (MASW, refraction), borehole velocity logging, and dynamic laboratory testing to define Vs profiles, amplification factors, and liquefaction potential. Delivers the design response spectrum and soil classification required for structural analysis under I.S. EN 1998-1.
Ground Improvement Seismic Verification
Pre- and post-treatment shear wave testing to confirm that vibrocompaction or stone column installations meet the stiffness targets assumed in the seismic design. We quantify the reduction in liquefaction susceptibility and the increase in Vs after ground treatment.
Quick answers
Does a low-seismicity area like Naas really need a seismic microzonation study?
The Irish National Annex to Eurocode 8 requires a seismic assessment for structures in importance class II and above, and the default ground type assumptions can be conservative—or unconservative—depending on local soil conditions. A microzonation study replaces generic factors with measured values, often reducing foundation costs while proving compliance.
What field tests do you run for a seismic microzonation in Naas?
We typically start with a MASW survey to capture the Vs30 profile across the site, followed by targeted boreholes with downhole or crosshole velocity logging. If liquefaction is a concern, we add SPT or CPT soundings to feed the Boulanger and Idriss cyclic resistance analysis.
What is the typical investment range for a seismic microzonation study in County Kildare?
The cost depends on the site size, the number of survey lines and boreholes, and the extent of dynamic laboratory testing. For a typical commercial or residential site in Naas, the study falls between €4,270 and €16,060, with the final figure driven by the geophysical array density and the complexity of the ground response modelling.