Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–3
Persistent slab avalanches are becoming harder to trigger, this does not however mean it will be impossible. Recent field observations continue to show signs of unstable snow including collapsing, shooting cracks, and propagating test results. Large triggers such as a small wind slab avalanche or a cornice fall may be required to initiate a persistent slab avalanche today however, shallow trigger points such as buried rocks or small trees are areas of concern for the backcountry traveler. These are areas where the weight of a skier/snowboarder may be enough to initiate slab failure. While the likelihood of triggering a persistent slab avalanche is very low, the consequence of doing so is high. Avalanches breaking on these lower week layers have the potential to be quite large and destructive.
Persistent Slab problems challenge our patience, and managing this problem requires extensive evaluation and deliberate terrain choice. Don’t be afraid to investigate the lower reaches of the snowpack to see if old snow is present in the areas you wish to travel. This may mean digging all the way to the ground if you suspect old snow is present. Remember that persistent slab avalanches often propagate across and beyond terrain features that would otherwise confine surface instabilities such as wind or storm slab. Persistent slab avalanches can be triggered from lower angle terrain, the bottom of a slope, and in some cases, remotely triggered from adjacent terrain. Give yourself a wide safety margin, be wary of hazards that may reside above you, and use terrain choice to limit your exposure.