Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1.5–2.5
Layers of weak snow in the upper snowpack can produce large, wide, 2-3' thick slab avalanches. You're most likely to trigger a slide involving these layers in areas where the wind has built a slab on top (read Problem #2 below). However, enough snow has fallen here that avalanches failing in terrain sheltered from the wind are a very real possibility. Avalanches that fail on these weak layers will be large and destructive, breaking significantly wider and deeper than a simple wind slab. You can trigger large avalanches on these layers from gentle terrain above, below, or to the sides of steep slopes, a process known as remote triggering.
Last week I spotted a large avalanche on Copper Mountain. It broke about 2 feet deep on a layer of weak facets. The slide appeared to have been remotely triggered by a skier on a low-angle ridge above a steeper slope (photo of the triggering track and crown). While the avalanche was initiated in wind-loaded terrain, crowns opened up in apparently sheltered terrain as well (photo at right/above). Friday on Copper, my snowpack tests returned repeated unstable results. A dense, 2+ foot thick slab failed cleanly and slid off into my lap with each test. The combination of a recent large natural avalanche, an ugly snowpack structure, and unstable snowpack test scores, was plenty of evidence to keep me out of big, steep, complex avalanche terrain. Additional snow and wind loading overnight have only made this problem worse.
The nature of these weak layers changes from slope to slope, but it's safe to assume that they exist on most slopes. Expect to find weak, sugary facets on shaded slopes and crust+facet sandwiches on slopes that face the sun. The best management strategy for this persistent slab problem is terrain management. Today I recommend you choose simple, conservative terrain to play in. Pay close attention to the terrain around you and above you, and spend some time contemplating the potential outcomes of being caught in an avalanche in the terrain you are in. Cliffs, trees, and terrain traps magnify the consequence of even small slides.
(2/28/2023) NE face of Copper Mountain at 8,400'. This avalanche appeared to be remotely triggered by a skier from above. This crown in sheltered terrain points to the potential for encountering avalanche problems outside of areas that are obviously affected by the wind.