Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2
Skiers and snowmobilers have triggered 4 large avalanches since last week's storm, many of them remotely (from a distance above, below, or to the side of a steeper slope). On Thursday, Chris investigated an avalanche near Galena Summit that was remotely triggered by skiers from flatter terrain above (video at right/above). The 5-12" of snow that fell near Galena Summit and Smiley Creek since Sunday night is enough to keep the snowpack on edge.
The culprit weak layers in all of these slides have been sugary facets buried 1.5-3 feet deep. The distribution and sensitivity of these layers are somewhat irregular. You are most likely to find them on slopes that face E-NE-N-NW above about 8000'. In this terrain, it's best to assume these layers exist and choose lower angled slopes not threatened by steeper slopes above. You're more likely to trigger persistent slab avalanches in areas where the wind has stiffened the snow surface or formed drifts, but they are possible in sheltered terrain as well.
Dealing with persistent weak layers is tricky business, particularly as they become more deeply buried. Snowpack test results become less reliable, and obvious signs of instability are typically absent. The first clear sign of an unstable snowpack may occur when you trigger a large avalanche. These types of slides can be triggered remotely—from a distance above, below, or to the side of a steeper slope.
ADDITIONAL DISCUSSION: Thin, soft, fresh wind slabs may exist in exposed, upper elevation terrain. Be alert to the consequences of triggering such a small to medium-sized slide in steeper, rocky terrain. These slabs are also adding stress to the weak layers of snow that are described above. Triggering even a small slide could help to trigger a thicker slab as snow flows down the slope.