Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 2–3
A dense, 2-4' thick slab overlies weak layers of sugary facets and facet+crust combinations. The weak layers are most common on middle and upper-elevation slopes facing SE-E-N-W. These weak layers are not as well-developed (i.e. "bad") as further south, and as a result, the avalanche cycle in this zone was not as extensive. Still, observers reported numerous large to very large avalanches in the aftermath of the storm.
Where does that leave us now? There is uncertainty surrounding how well the weak layers are adjusting to this unique loading event. Further, our conditions are best described as low probability/high consequence with the following characteristics:
- You aren't likely to experience signs of instability such as cracking and collapsing.
- Snowpack tests don't work well with dense slabs approaching 3' in thickness.
- Multiple people might ride on a slope before it avalanches.
- Any slide triggered could be large enough to be unsurvivable.
While conditions in this zone are (relatively) less dangerous than further south, the uncertainty of how our snowpack is stabilizing and the possibility of triggering a catastrophic avalanche do not inspire confidence. Despite the MODERATE danger rating, a conservative approach remains the best bet. Stick to moderate slope angles (less than about 35 degrees), avoid obvious starting zones, and pay attention to what would happen if you triggered an avalanche.
ADDITIONAL DISCUSSION
- While weather stations didn't record impressive winds with yesterday's storm, I observed moderate winds transporting snow near Copper yesterday. Watch for fresh drifts in upper elevation, wind-exposed terrain.
- Despite the wintry weather, spring is officially here. As such, even brief periods of sunshine today could be intense enough to trigger loose snow avalanches on steep, sunny slopes.
(3/12/2023) This avalanche failed on a SE slope at 9000' in Lola Creek. Based on the aspect and the appearance of the crown, this slide likely failed on a layer of facets below a melt freeze crust.