Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
In the Southeast Mountains, the last round of persistent slab avalanches occurred on March 16th. As snow surfaces refreeze following a week of warm weather, concerns for this problem on shoulder aspects will be even further reduced. The most prominent weak layers are surface hoar buried a couple of feet deep and depth hoar near the ground. Persistent slab avalanches can be remotely triggered from low-angle terrain and break deeper and wider than you might expect. Triggered slab avalanches are unlikely on mid to low-elevation, southerly aspects, or areas where the snowpack is consistently deeper than 200 cm. Slope angles consistently less than 30 degrees are a reliable way to avoid the problem.
A large persistent slab on Mt. Crested Butte that ran on 3/16. This slope is shallow, variable in depth, and on the north half of the compass: a combination of ingredients you want to avoid.
Photo: Zach Guy