Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Today's snowfall and wind-drifting will stress weak, faceted snow buried 2-3 feet deep. This weak layer has been the culprit in almost all of the avalanches we've observed this season. You are most likely to trigger persistent slab avalanches where the snowpack is thinner, such as steep, rocky, upper elevation terrain that is affected by the wind. The snowpack is also thinner in the mountains near the mouths of the major drainages near Smiley Creek.
We continue to receive reports of obvious signs of instability near the edge of this zone. Some recent, obvious red flags:
- Multiple groups experienced large collapses and chose to stick to low angle slopes.
- Riders in the White Clouds experienced shooting cracks that shattered entire slopes.
- Chris found an unstable snowpack structure and his snowpack tests returned unstable scores (video at right/above) this weekend near Pole Creek.
- Ben found an unstable snowpack, experienced cracking and collapsing, and got repeated unstable snowpack test scores this weekend in the Owl Creek drainage.
- Observers near Galena Summit continue to report unstable snowpack test scores and a poor snowpack structure.
Be very careful today. This storm will increase the chance of triggering thick, destructive avalanches. Also, natural or human-triggered wind slab avalanches (see Problem 2 below) or large sluffs could "step down", triggering larger persistent slab avalanches as they move downhill. Given the possibility of remotely-triggering slides, avoid terrain with large, steep slopes above you.