Coquitlam sits on a complex mix of Vashon glacial till, Capilano sediments, and softer alluvial deposits along the Coquitlam and Pitt Rivers. That means you can hit dense, overconsolidated silts at 12 feet in one borehole and find loose, saturated sands at the next lot 200 meters away. When a geotechnical report calls for SPT N-values to confirm bearing capacity near Riverview or along the Lougheed corridor, we mobilize a CME-75 rig and run the test per ASTM D1586. The triaxial lab data often supplements field N-values where silt content is borderline, and we pair the SPT with CPT soundings when the stratigraphy needs continuous profiling without sample disturbance.
A raw N-value of 12 in loose alluvium corrected to (N1)60 of 9 — that's the difference between designing for liquefaction or not in Coquitlam's seismic zone.
