One of the most persistent mistakes we see in St. Albert is treating the river valley slopes as uniform clay till, when in reality the stratigraphy can shift from dense till to soft lacustrine deposits within a single lot. A generic desktop study won't catch that. We provide slope stability analysis that begins with site-specific drilling and lab testing, because the failure mode on a 4:1 slope backing onto the Sturgeon River is fundamentally different from what you'd design for a shallow embankment in a flat subdivision. When the project involves retaining walls or deep cuts near the river terrace, integrating our retaining wall analysis with the slope model prevents the kind of compound failure that standard software misses when boundary conditions are simplified.
A slope that stands through a dry August in St. Albert has very little to say about how it will behave during the first significant thaw cycle in March.



