The 28 November 2020 Landslide, Tsunami, and Outburst Flood – A Hazard Cascade Associated With Rapid Deglaciation at Elliot Creek, British Columbia, Canada
Marten Geertsema, Brian Menounos, Gemma Bullard, Jonathan L. Carrivick, John J. Clague, Chunli Dai, Davide Donati, Göran Ekström, Jennifer M. Jackson, Patrick Lynett, Manuele Pichierri, Andy Pon, Dan H. Shugar, D. Stead, Justin Del Bel Belluz, Pierre A. Friele, Ian Giesbrecht, Derek Heathfield, Thomas H. Millard, S. Nasonova, A. J. Schaeffer, Brent Ward, Debi Blaney, E. Blaney, Camille Brillon, Christian Bunn, William C. Floyd, Bretwood Higman, Katie E. Hughes, W McInnes, Kriti Mukherjee, M. Sharp
Abstract
Abstract We describe and model the evolution of a recent landslide, tsunami, outburst flood, and sediment plume in the southern Coast Mountains, British Columbia, Canada. On November 28, 2020, about 18 million m 3 of rock descended 1,000 m from a steep valley wall and traveled across the toe of a glacier before entering a 0.6 km 2 glacier lake and producing >100‐m high run‐up. Water overtopped the lake outlet and scoured a 10‐km long channel before depositing debris on a 2‐km 2 fan below the lake outlet. Floodwater, organic debris, and fine sediment entered a fjord where it produced a 60+km long sediment plume and altered turbidity, water temperature, and water chemistry for weeks. The outburst flood destroyed forest and salmon spawning habitat. Physically based models of the landslide, tsunami, and flood provide real‐time simulations of the event and can improve understanding of similar hazard cascades and the risk they pose.