Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Several weak layers are buried in the upper 1-3' of the snowpack. These layers are capable of producing large avalanches. I went looking for them in this zone on Friday and found them in multiple snowpits (read my observation and see photos). These weak layers vary by aspect and elevation, and the overlapping patterns are complex and hard to decipher. In this zone, these layers appear to be most reactive on slopes that face the sun, where crusts with facets on top exist. However, we've seen avalanches and unstable snowpack test scores on shaded slopes as well. Crusts, facets, surface hoar—it's a safe bet that one or more of these layers exist on most slopes.
These layers are capable of producing large avalanches, but the likelihood of triggering a slide is gradually decreasing. Unfortunately, the structure for producing these slides (slab + weak layer) remains. Want to avoid triggering a large avalanche today? You can significantly reduce your risk by steering clear of steep, wind-affected terrain.
ADDITIONAL DISCUSSION: Weak snow makes up the base of the snowpack here. In most places, it is buried beneath a thick, dense slab of snow, and impacting it with your weight is unlikely. However, the two large avalanches triggered by skiers in this zone in the past 8 days are proof positive that this weak snow should remain on your radar. You are most likely to trigger an avalanche involving this snow in steep, rocky, wind-affected terrain where the slab over this weak snow is thinner and the weak layer is more "accessible". Smaller slides can break down into deeper weak layers, producing a larger, more destructive avalanche.
(1/1/2023) Debris from a very large avalanche that was remotely triggered above Hyndman Creek in the Pioneer Mountains. This slide failed in a heavily wind loaded area and very likely involved a persistent weak layer. It covered the summer trail with a pile of debris that was 100-150' wide and 4' deep.