It is possible by measuring stress conditions within the slope during failure. Pressure cell can be placed along the critical failure circle and measure stress conditions. I suggest you to read any experimental technique related books.
maybe by sacrificing a small segment of the slope, and overloading it with added weight? That would preserve the "in-situ" condition, and the scarified slope can be relatively large (preserving the layers).
Otherwise... making a slope of the same geometry and testing it in a centrifuge. But that would sacrifice the "disturbed soil states" plausibly present in the original slope. And layering can be hard to capture.