A six-story mixed-use project near North 27th Street hit sandstone at 18 feet. The contractor expected shale. The excavation plan changed overnight. We set up inclinometers and survey points before the next cut. That kind of surprise is normal in Billings. The geology shifts fast here. You get river terrace gravels near the Yellowstone. You get fractured sandstone on the Rims. And you get expansive clay in the Heights. Our team tracks wall deflection, vibration, and groundwater levels so the project keeps moving. A deep excavation analysis paired with real-time monitoring gives the superintendent hard data, not guesses. The Yellowstone River aquifer adds another variable. Dewatering changes pore pressure. We measure it. No two sites behave the same way here. That is why we stay on site until the shoring is complete and the readings are flat.
In Billings, the sandstone-to-colluvium contact on the Rims creates wedge failure risks that standard monitoring can miss.



