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  • 19 minutes ago
Officials in Washington State are assessing updated tsunami models for San Juan County in light of a possible earthquake originating from the Alaska-Aleutian subduction zone. The projections indicate wave heights ranging from 3 to 10 feet across the San Juan Islands, with particularly elevated levels anticipated near Eastsound. Brendan Cowan, the Emergency Management Director, noted that while the modeled flooding is minimal, strong currents may pose risks to docks and other structures. According to guidance for a Cascadia Subduction Zone event, a tsunami could reach the area within 45 to 90 minutes. Authorities are actively enhancing local preparedness strategies and inundation resources.
Disclosure:This video contains stock footage and content created or enhanced using Ai-assisted tools ai-generated

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00:00Washington state officials are reviewing new tsunami modeling for the San Juan Islands.
00:04The model examines a potential earthquake in the Alaska Aleutian subduction zone.
00:09It shows wave amplitudes of 3 to 10 feet across the islands.
00:14East Sound has some of the highest measurements in the new model.
00:17Officials say the modeled inundation would be relatively limited.
00:20However, strong currents could still threaten waterfront infrastructure.
00:24Friday Harbor's docks could face complications from floating debris and currents.
00:28Emergency Management Director Brendan Cowan says residents should head uphill.
00:33He says high ground is generally close to homes across the county.
00:37A Cascadia subduction zone earthquake poses a different level of concern.
00:41County guidance says a tsunami could arrive within 45 to 90 minutes.
00:45Some high-risk areas could see water reach 20 feet above mean high tide.
00:50Officials say preparation is important because the islands could become isolated.
00:54More tsunami information will be added as the latest model is reviewed.
00:59Disclosure.
01:00This video contains stock footage and content created or enhanced using AI-assisted tools.

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