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Massive Alaska megatsunami was second largest ever recorded

Researchers used satellite and seismic data to reconstruct a landslide-generated wave that climbed 1,578 feet, the second-highest tsunami ever recorded.

  • On Wednesday, researchers led by University of Calgary geomorphologist Daniel Shugar published a study in the journal Science reconstructing a mega-tsunami triggered by a massive landslide into Alaska's Tracy Arm Fjord on August 10, 2025.
  • Rapid warming caused the South Sawyer Glacier to retreat about 500 metres, destabilizing the mountainside and unbuttressing 370 million metric tons of rock that collapsed into the fjord.
  • The resulting wave reached about 481 metres, the second-highest run-up ever recorded, as debris fell 1,000 vertical metres into the deep, narrow fjord.
  • Cruise lines have suspended routes into the fjord this year, while Shugar described the event as a "good wake up call" given the fortunate absence of vessels near the slide.
  • Experts warn that continued glacier retreat and expanding tourism infrastructure increase the likelihood of future disasters, necessitating better slope monitoring and proactive policymaking to mitigate risks.
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hna.dehna.de
+2 Reposted by 2 other sources
Center

The tsunami hit Alaska last summer. A landslide triggered a wave that was one and a half times as high as the Eiffel Tower.

Center

The tsunami, documented by Science magazine, hit Alaska last summer. A landslide caused a wave high once and a half the Eiffel Tower

·Italy
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Center

A group of American scientists have revealed that a huge wave, in fact a megatsunami that was generated when an Alaskan mountain collapsed in the sea, is the second highest recorded in history.It happened last summer, when a giant wave swept away a remote fjord in southeast Alaska, razing everything it found in its wake.At that time the event went virtually unnoticed, but a new scientific analysis has now shown that it was caused by a massive la…

·Madrid, Spain
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ucalgary.ca broke the news on Tuesday, May 5, 2026.
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