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Edition 1
The Oso Landslide · 26 July 2026 · Current published edition
Field-by-field comparison
Initial edition
The Oso Landslide
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At 10:37 a.m. on 22 March 2014, a large portion of a historically unstable slope collapsed near Oso, Washington. Debris crossed the North Fork Stillaguamish River, spread across about one square mile, buried the Steelhead Haven neighborhood and State Route 530, and killed forty-three people. The slide's extraordinary mobility left almost no warning between collapse and impact.
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22 March 2014
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State Route 530 landslide and Steelhead Haven area
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The Hazel slope contained deposits from previous landslides and had failed repeatedly, including in 2006. Studies and maps described landslide hazards, but terminology, boundaries, recurrence, and implications were not consistently communicated to residents or land-use decisions. An unusually wet early 2014 raised groundwater, while river erosion and slope geometry also influenced stability.
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A deep-seated block on the upper slope moved and disintegrated into water-saturated debris. Material struck older slide deposits, crossed the river, and accelerated across the flat valley farther than many expected. The entire destructive sequence took only minutes, overtaking homes before residents could receive or act on any warning.
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The slide dammed the river, flooded upstream, and cut the highway and communication routes. Neighbors and firefighters entered unstable mud immediately, followed by regional urban-search teams, geologists, excavators, dogs, and volunteers. Recovery continued for months under rain, groundwater, biohazards, sharp debris, and risk of additional slope movement.
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Washington improved geological mapping, landslide inventory, emergency coordination, and public risk communication while debates continued over logging, permitting, warnings, and liability. The highway was rebuilt and a permanent memorial opened in 2024. Scientific work refined understanding of landslide mobility and how previous deposits can be remobilized.
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Oso shows the gap between knowing that a slope has failed before and conveying what future failure could do. Hazard maps must communicate runout, uncertainty, and decision consequences in language residents and officials can use, not only mark a technical polygon.
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The SR 530 Slide Memorial, restored highway, altered river, bare and revegetating scar, surviving trees, recovered objects, lidar maps, geotechnical records, oral histories, and volunteer archives preserve the event. Memorial and private areas require respectful access.
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Scientists agree that groundwater and preexisting landslide geology were central, while the relative roles of rainfall, river erosion, logging, and other factors remain debated. Statements that the slide was wholly unforeseeable or definitely caused by one land use overstate the evidence. Forty-three deaths are established.
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Chaos Tourist editorial
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2014 Oso mudslide
SR 530 Landslide Commission Final Report
SR 530 Slide Memorial
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At 10:37 a.m.
A deep-seated block on the upper slope moved and disintegrated into water-saturated debris.
Scientists agree that groundwater and preexisting landslide geology were central, while the relative roles of rainfall, river erosion, logging, and other factors remain debated.
Oso shows the gap between knowing that a slope has failed before and conveying what future failure could do.