Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1–2.5
1 to 3-foot stiff cohesive slabs from December and January snow and wind events rest on top of facets and depth hoar near the ground that formed earlier in the season. In most pits, these layers have been found under an obvious rain crust from early December and continue to remain weak and fragile in the overall shallow snowpack that currently exists. Don't be lured into thinking the lack of signs of unstable snow like shooting cracks and loud audible collapses means the slope is safe. Taking the time to dig a quick pit is a great way to see if the strong over weak layering exists on the slope you plan to play on. Although the likelihood of triggering an avalanche has been slowly decreasing since the last loading event, the consequences still remain high as any avalanche triggered could be large as it fails near the ground leading to a nasty ride through rocks and trees.