Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–3
In the Northwest Mountains, high-consequence slabs breaking on older weak layers have become isolated and difficult to trigger. Any lingering persistent slabs are most likely triggered from an unusually shallow or previously wind-eroded slope where the total snowpack height is below average. Large cornice falls could act as triggers as well. Persistent slab avalanches can be remotely triggered from low-angle terrain and break deeper and wider than you might expect. The most problematic structures are on shallower slopes on the north half of the compass. Slope angles consistently less than 30 degrees are a reliable way to avoid the problem when in doubt.
The crown of a very large persistent slab remotely triggered by snowmobiles on March 8. This slope is west facing and eroded by seasonal winds, making for a shallower and more problematic snowpack than other slopes.