Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
The primary avalanche concern is a weak layer of faceted snow formed during the December dry spell and buried on 12/25. This layer is about a foot below the surface on slopes facing W-N-E-SE. While the weak layer is widespread, the overlying slab is not—and both are needed to create an avalanche.
The most suspect terrain is northerly aspects near treeline. Above treeline, strong northerly winds have created an erratic pattern of slab distribution, stripping snow from many north and east aspects typically loaded with it. Cross-loading remains a factor, meaning you could move from scoured, benign-looking terrain to standing atop a hard slabs resting on weak facets.
Watch for changes in surface texture, such as rough and thin transitioning to smooth, hard, and thick. Pay close attention to gullies, depressions, and leeward sides of terrain features, as these are common deposition zones.
In these same areas, there is a lingering chance for avalanches to fail on weak facets near the ground. To mitigate this risk, avoid extreme, rocky slopes with a thin snowpack.