Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1.5–2.5
A complex patchwork of weak layers exists in the upper 1-4' of the snowpack. Yesterday, skiers in the Smiley Creek drainage reported triggering a large slide that broke 2 feet deep in wind-sheltered terrain. This was the fourth reported human-triggered avalanche involving these layers in the past 5 days. On slopes that face away from the sun, you'll find layers of surface hoar and weak facets. On slopes that face the sun, you'll find crusts with facets on top, and some spotty surface hoar mixed in. It's a safe bet that most slopes have one or more of these weak layers.
The likelihood of triggering a slide on these weak layers depends on how deeply buried they are and the nature of the slab on top of them. Weak layers closer to the surface are easier to impact with your weight. Deeper weak layers are harder to impact, but the resulting slide will be much larger and more destructive. You're most likely to trigger avalanches on slopes where the wind has formed drifts or slabs or stiffened the snow at the surface (example). But, as yesterday's slide in Smiley Creek illustrates, these avalanches are also possible in sheltered terrain.
Pay close attention to the snow you are moving through: cracking and collapsing are obvious signs of instability. But, don't expect to get direct feedback today. Persistent slab avalanches behave in ways that catch experienced backcountry travelers off guard. The first sign of instability may be an avalanche that you trigger. These slides can break wider than you expect and can be triggered long distances away from steeper slopes.
ADDITIONAL DISCUSSION: Weak snow exists near the base of the snowpack. Triggering slides on this snow is unlikely, but the possibility can't be ruled out in steep, rocky, wind-affected alpine terrain. Slopes like these have variable snow depths, and thinner snowpack areas allow us to more easily impact deeply buried weak layers.
(1/12/2023) A small, likely skier-triggered avalanche near Galena Pass. Two sets of ski tracks were observed near the crown. The avalanche released on a thin layer of facets sitting atop a crust. NE aspect at 8,800'.