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A 481-meter-high landslide-tsunami in a cruise ship-frequented Alaska fjord
Dan H Shugar1, Katherine R Barnhart2, Mira Berdahl3
1Water, Sediment, Hazards, and Earth-Surface Dynamics (waterSHED) Lab, Department of Earth, Energy, and Environment, University of Calgary, Calgary, AB, Canada.
Abstract:
Early in the morning of 10 August 2025, a >64 × 106-cubic meter landslide struck Tracy Arm fjord in Alaska. The landslide was preconditioned by glacial retreat caused by climate change. The resulting 481-meter runup megatsunami followed an initial 100-meter-high breaking wave traveling at >70 meters per second. The landslide was preceded by several days of microseismicity, which increased in rate and magnitude until ~1 hour before failure. The landslide produced globally observed long-period seismic waves equivalent in size to a moment magnitude 5.4 earthquake. A long-period (~66 second) global seismic signal, produced by a landslide-induced seiche trapped within the fjord, persisted for up to 36 hours, the second time a days-long seiche had thus been observed. With fjord regions increasingly visited by cruise ships, and climate change making similar events more likely, this unanticipated, near-miss event highlights the growing risk from landslides and tsunamis in coastal environments.
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