Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 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 neighboring zones the past few days and found them. You can read my observation and see photos from Baker Creek and the East Fork of the Big Wood to find out more. These weak layers vary by aspect and elevation, and the overlapping patterns are complex and hard to decipher. Crusts, facets, surface hoar—it's a safe bet that one or more of these layers exist on most slopes.
We received a report of a small avalanche that was remotely triggered yesterday by a rider (photo here). Little else is known, but remotely triggered slides generally fail on the types of weak layers described here.
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.
(12/31/2022) This large avalanche was remotely triggered from hundreds of feet away on 12/31. It failed on a S-facing slope at 9,500' near Mushroom Ridge, which is near Galena Summit.