Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 2–3
Even though the weaknesses within the storm snow may consolidate quickly as the storm tapers off, persistent weak layers like buried surface hoar (weak feathery snow crystals) and facets (weak sugary snow) still lurk at the base of the storm snow. The storm snow will become more of a slab above these old layers, shifting the storm slab problem to a persistent slab problem. In some cases, weak layers may still lurk below the old snow surface, especially in the eastern and southern parts of the forecast area. These layers will take extra time to adjust to the new load. Significant uncertainty remains regarding which slopes may have already avalanched and where these weak layers may remain. This uncertainty makes even larger safety margins even more important.
People can trigger persistent slab avalanches from a distance while traveling below or next to a slope in lower-angle terrain. They also may not release until a person has committed to a slope. These avalanches can also break much wider than expected and may occur in sheltered terrain that people typically consider "safer." The persistent weak layers may also lurk in more exposed terrain where wind-blown snow has created a much thicker slab. Expect large to very large avalanches several feet deep when these old, weak layers of snow fail.
(2/13/2025)
We triggered this avalanche from flat terrain near the spot Steve is standing about 50-100 ft away from the avalanche on an E-NE facing slope at 7900 ft on Andesite Ridge.
Photo: Sierra Avalanche Center