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The document analyzes the mechanism of failure of the Mount Polley Tailings Storage Facility, which experienced a breach on August 4, 2014, due to foundation failure. It highlights the role of three-dimensional stability effects and strain-weakening in the failure process, particularly within a thin shear band in the glaciolacustrine unit at the base of the slide. The findings suggest that significant weakening of the Upper GLU material was necessary for the initiation of the breach, raising questions about

Author

Prince kojo Nyame

Language

EN