Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
A well-identified weak layer (buried surface hoar) is down about 2' at mid-elevations and found just above a prominent crust (2/13) in the upper snowpack. This layer was found on some shady aspects in the Hurricane Ridge area, including near ridgelines and also in snow pits on Mt Ellinor. A sensitive snowpack with collasping and whumpfing was observed in the Hurricane Ridge area earlier in the week, but not on Thursday and Friday. While triggering a persistent slab avalanche in the Olympics may not be likely, the consequences could be deadly.
Treat all open steep slopes as suspect until proven otherwise, especially shady aspects where surface hoar was more likely to have survived and buried intact. If you experience any collapsing or whumpfing, remotely trigger avalanches, or see other signs of instability, retreat to simpler terrain. Stick to shaded, wind-sheltered terrain and slopes under 35 degrees.
Persistent slabs are notorious for surprising backcountry travelers; they break more widely across the slope and can be triggered from lower-angle terrain than run-of-the-mill storm slab avalanches. Dig and look for the buried surface hoar to help rule out slopes, and consider using snowpack tests to gain more information, but do not use inconclusive results to deem a slope "safe" or not.
(2/26/2026)
A propagation saw test (PST) result of 79/100. End on an N aspect near Steeple Rock. This snowpack test gauges the likelihood of a fracture to propagate on a known weak layer (buried surface hoar). Numbers below 50 indicate a higher likelihood of fracture propagation.
Snowpack tests like this can be helpful for identifying which slopes to avoid, but they are only one piece of information from a single location. They should not be used to deem a slope "safe".
Photo: Sam Luthy - NPS