Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
Avalanche conditions will remain similar to yesterday. Light to moderate snowfall will continue to add load and build slab depth over weak snow. Dangerous avalanche conditions exist. Human-triggered avalanches are likely, and could be 1–2+ feet deep. In steep, rocky terrain and in areas with a thinner snowpack, avalanches may step down into deeper weak layers in the snowpack (see Problem 2).
On the north side of Thompson Pass, 1-2 cm buried surface hoar over a rain crust continues to be found up to 3000’. In most areas we’ve observed, the buried surface hoar has been flattened/laid over, except north of our Continental zone, where it has remained more intact. As the slab above this layer stiffens and thickens, expect longer propagation and the potential for larger, more connected releases. A few small natural avalanches have recently been observed on steep rollovers in the Python Buttress area. In the Maritime zone, buried surface hoar is no longer widespread due to warm temperatures and rain.
Above 3000’, buried surface hoar has not been identified, but a reactive interface exists. On 2/6, two separate skier-triggered avalanches at upper elevation propagated widely for the terrain and resulted in full and partial burials on different aspects. See the Observation section for details.
Travel advice: The best way to manage this problem is to avoid complex terrain and slopes steeper than 30°. Both incidents occurred with no obvious warning signs beforehand. Snowpits are not a reliable assessment tool for this problem—small differences in slab thickness or stiffness can greatly change sensitivity.
(2/6/2026)
Skier triggered avalanche on Girls Mountain/ 6000'/ E/NE. Fracture character connecting through the rocks along with a sympathetic avalanche on the lookers left of the photo indicate a persistent grain at the interface.