Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Expect to find 1-2.5 foot thick slabs in areas sheltered from the wind. The slab may be twice as thick in terrain affected by the wind. These avalanches have failed on various weak layers: facets and/or surface hoar on shadier aspects and crust + facet combinations on sunnier slopes. Large natural and human-triggered avalanches have occurred on several aspects in recent weeks. Assume this problem exists on all upper and middle elevation slopes and on shadier, lower elevation aspects.
Avalanches on this uncommonly widespread and fragile layer will break widely and in surprising ways. Don't expect obvious signs of instability, like snowpack cracking and collapsing. Your first sign of trouble may be the destructive avalanche you trigger. These slides can be triggered from long distances away—from flat or gentle terrain below, above, or to the sides of steep slopes.
(1/19/2024) This photo shows several large avalanches that were remotely-triggered by riders in the Beaver Creek drainage. The furthest away slide is over 800 feet wide, and failed a half mile from where the avalanches were triggered, out of sight on the right side of the photo.