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. Mid to low-elevation, southerly aspects have the most trustworthy snowpack. 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.