The most expensive mistake we see in Eugene? Assuming the silty clays near the Willamette River behave like the gravels up on the McKenzie fan. They don’t. A contractor pours a standard footing based on a cheap desktop study, and two winters later the floor slab cracks along a diagonal—differential settlement from a buried peat lens nobody knew was there. The Oregon Department of Geology and Mineral Industries (DOGAMI) has mapped significant portions of the valley floor as moderate-to-high liquefaction susceptibility, which makes continuous profiling essential. In Eugene, where the average annual rainfall of 46 inches keeps the water table high from November through April, a CPT test gives us the real stratigraphy—tip resistance, sleeve friction, and pore pressure—without the sample disturbance that plagues split-spoon methods in soft, saturated ground.
In Eugene’s saturated valley soils, a 15 cm² cone with pore pressure measurement catches thin sand seams that standard SPT intervals miss entirely.
