Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
Weak snow at the base of the snowpack drives the primary avalanche concern today. A 1.5-2.5 thick slab of dense snow rests uncomfortably on top of this weak snow. This combination of slab + weak layer exists on all upper elevation slopes and on shaded middle elevation slopes (those facing E-N-W). If you dig down on shaded slopes you'll find an obvious layer of very weak snow near the ground. On slopes that face the sun you'll find a less-obvious layer of small facets on top of a stout melt-freeze crust
As the days tick by without significant loading, obvious signs of instability have decreased. Reports of large collapses have become much less frequent and the most recently observed large avalanche failed roughly 3 weeks ago. The likelihood of triggering one of these slides is decreasing, but not going away. Tracks on a slope are not an indication that the slope is stable — avalanches may be triggered after many riders have crossed a slope.
You can eliminate your risk of encountering one of these large slides by steering clear of avalanche terrain harboring this combination of slab + weak snow. If you are planning to enter avalanche terrain, spend a bit of time thinking about the consequences of triggering a slide. Slopes with terrain traps at the bottom and with trees and rocks that you can get dragged through amplify the consequences of triggering an avalanche.