Water Stewardship Information Sources

ID 1825
Citation Cuervo V., Burge L., Beaugrand H., Hendershot M., Evans S.G. (2017) Downstream Geomorphic Response of the 2014 Mount Polley Tailings Dam Failure, British Columbia. In: Miko_ M., Vilímek V., Yin Y., Sassa K. (eds) Advancing Culture of Living with Landslides. WLF 2017. Springer, Cham. https://doi.org/10.1007/978-3-319-53483-1_33
Organization SNC-Lavalin Inc; University of Waterloo; Stantec Consulting Ltd; Okanagan College
URL https://link.springer.com/chapter/10.1007/978-3-319-53483-1_33
Abstract/Description or Keywords On August 4, 2014, the failure of the Tailings Storage Facility dam at the Mount Polley copper and gold mine in British Columbia (Canada) produced a dynamic and complex geomorphic response downstream. The dam breach was caused by rotational sliding of the embankment due to foundation failure, resulting in sudden loss of containment of water and tailings. The released volume was estimated to be 25 Mm3. The resulting flow traveled approximately 9 km down the Hazeltine Creek valley over a vertical elevation of 205 m. The August 2014 event is the largest tailings dam failure recorded in Canada and the second largest recorded globally in the last decade. This investigation documents and analyzes the general downstream geomorphic response of the event in the Hazeltine Creek channel and floodplain. It utilizes an integrated approach of geomorphological mapping, topographic analysis, historical aerial photograph analysis, and field surveys to identify and quantify the geomorphic impacts of the event. Overall results indicate that these impacts are significant and comparable to those resulting from extreme debris flow and outburst flood events in mountainous environments in Canada and worldwide. Tailings dam failure; Flow failure; Debris flows; Outburst flood; Geomorphic impacts; Hazard and risk
Information Type Article
Regional Watershed Quesnel River
Sub-watershed if known Hazeltine Creek
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