Register · Events
How the 2014 Oso landslide dammed a river and cut a Washington highway
The Oso landslide killed 43 people on 22 March 2014 and blocked the North Fork Stillaguamish River and State Route 530. Water overtopped the debris dam within about 25 hours. The river cut a new channel while road crews worked to restore access.
Sources checked
- 22 March 2014Landslide crossed the valley
The slide near Oso travelled almost two kilometres. Its deposit crossed State Route 530 and blocked the North Fork Stillaguamish River. · Landslide Source 1
- 23 March 2014River overtopped the deposit
Water began flowing over a low part of the deposit within about 25 hours of the landslide. · River Source 2
- 24 March 2014Aerial surveys measured the site
The USGS assessment lists lidar at one-metre horizontal resolution and aerial imagery at 0.3-metre resolution for this date. · Survey Source 1
- 26 March 2014Crews opened an alternate access route
State and county crews cleared the Mountain Loop Highway as work also connected State Route 530 with a utility road for responders. · Road and access Source 3
- Early April 2014Pilot channel excavated
County and cooperating agencies cut a pilot channel in the eastern part of the deposit to speed drainage during the search effort. · River and response Source 1
- 25 April 2014Piloted public access contracted
Washington State Department of Transportation contracted work to guide public traffic on a separate utility access road. · Road and access Source 3
Show 7 more dates
- May 2014River channel re-established through the deposit
A USGS study reports a deeply inset channel 20 to 40 metres wide through the deposit by May. · River Source 2
- 30 May 2014Highway clearing completed
The county project account records about 127,000 tons of debris moved during the State Route 530 clearing project. · Road and access Source 3
- 31 May 2014Highway reopened to piloted traffic
State Route 530 reopened through the area to one-way piloted traffic. · Road and access Source 3
- 1 June 2014Standing pool receded at lower flows
USGS reports that by this date no standing pool remained at river flows below about 57 cubic metres per second. · River Source 1
- July 2014Water surface approached its earlier profile
USGS found the channel water surface about one metre above its pre-landslide profile. · River Source 2
- 22 September 2014Highway reconstruction substantially complete
The state recorded substantial completion of the emergency roadway reconstruction project. · Road and access Source 3
- First 18 monthsSediment moved downstream
USGS estimated 820,000 metric tonnes of sediment eroded from the deposit into the river over the first 18 months. · River Source 2
Choose a milestone to trace the first day, the river’s changing channel or the return of road access.
The deposit created a temporary lake
The preliminary USGS assessment estimated an impoundment about eight metres deep, three kilometres long and holding about 3.3 million cubic metres of water. Once it overtopped, the river began cutting into the deposit through a new channel. Source 1
The water surface fell as the new channel deepened
USGS reports that average water-surface elevation through the deposit fell about seven metres over roughly two months. By July 2014 it was about one metre above the pre-landslide profile. The profile and the persistence of a standing pool were separate indicators of the river's change. Source 2 Source 1
The highway reopened in stages
The May reopening allowed one-way piloted traffic after road-clearing work. The project account separately dates substantial completion of emergency reconstruction to 22 September. A date for limited access describes a different stage from completing the reconstruction contract. Source 3
Sediment continued moving after the initial response
The 18-month study estimates that erosion from the deposit delivered about 820,000 metric tonnes of sediment to the river. It estimates that silt or clay made up 77% by mass. Road-clearing debris figures describe material moved by crews under a separate project. Source 2 Source 3