Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
Strong winds created stiffer slabs over the weekend. As temperatures cooled off, the winds ramped down and these slabs may be hidden by softer new snow. These slabs rest on a layer of faceted grains, surface hoar and crusts. The strongest crust at the base was buried in late January. If an avalanche breaks on this layer it could be 1.5-2ft+ deep, and potentially fracture across terrain features.
Because of the nature of these weak layers, avalanches could be triggered from adjacent slopes. The most likely place to trigger one of these would be beneath heavily loaded ridgelines and below large cliff outcroppings. Whumphing collapses are signs of instability to heed. Targeted snow profiles can identify the weak structure, look for it on shaded aspects above 6,000ft. To avoid the problem, you can stick to lower angled and sheltered slopes, away from larger terrain features.
(2/26/2024) There are a few sets of tracks that are barely visible. One of which comes right into the crown line. Photo: John Barkhausen