Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–3
Triggering 2-4 foot thick avalanches remains possible, especially in recently wind-loaded terrain. The snowpack has not fully adjusted to the weight of the February storms, and recent wind loading has kept some slopes teetering on the edge. Avalanche activity has been focused on the northern 2/3 of the compass (W-NW-N-NE-E-SE) in middle and upper elevation terrain, failing on faceted snow (commonly associated with crusts) buried about 2-4 feet deep. On SW and S aspects, we've observed less Persistent Slab activity but can't yet rule them out.
These avalanches can release in surprising ways. You can trigger them from flat or low-angle terrain long distances away from steep slopes, and they can break far above you. Several riders or skiers could safely ride a slope before someone triggers a slide. You may or may not experience snowpack collapsing or other obvious signs of instability before triggering an avalanche.
Unfortunately, snowpack stability tests will not conclusively determine if a given slope will or will not produce a Persistent Slab avalanche. If your primary goal is to not get caught in an avalanche, staying off of and out from below steep slopes is the most reliable way to reduce your risk.
Observations indicate these avalanches are most likely as you move to the southern, eastern, and northern portions of this zone, away from Galena Summit.