A recent commercial project along McGill Road hit unexpected fill at just over a meter deep, something the desktop study completely missed. That is the reality of building in Kamloops, where the valley floor conceals decades of backfill, old creek channels, and lacustrine silt layers deposited by glacial Lake Thompson. The exploratory test pit cuts through the guesswork. An excavator opens a trench to depths of 2.5 to 4 meters, and our geotechnical team logs the stratigraphy, takes bulk samples, and conducts in-situ density checks right there in the trench. For foundation designers working in the arid B.C. Interior, where colluvial fans spill off the surrounding benchlands, direct visual inspection of the subsurface often reveals more than a borehole log alone. We integrate the findings with a grain size analysis to quantify the silty sand composition typical of the South Thompson River terraces.
A single well-logged test pit in Kamloops can replace three speculative boreholes when the geology is layered and visually distinctive.
