The biggest mistake we see in Richmond Hill projects is assuming uniform soil. You hit a dense till layer at 3 meters and think you’ve got bearing capacity sorted. Then a sand lens appears at 6 meters and the N-value drops to 6. We’ve pulled split spoons across the Oak Ridges Moraine for years. The stratigraphy here is chaotic: glaciolacustrine silts, sandy tills, and the occasional buried river channel. A standard penetration test is the only way to get a true vertical profile when granular lenses hide between cohesive layers. We run the SPT with a calibrated automatic trip hammer on a CME-75 rig. Every sampler is driven exactly 450 mm. We record the blow count for each 150 mm increment. The N-value you get is real, not a guess. For sites near the kettle lakes, we often pair SPT with CPT testing to cross-check pore pressure dissipation in silty zones that might liquefy under seismic load.
N-values alone are just numbers. The real value is knowing which till layer you’re in and whether it will drain or trap water under your foundation.
