Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 3
A persistent weak layer (PWL) of faceted snow and depth hoar exists in the bottom foot of the snowpack on mid and upper-elevation slopes primarily facing west, north, and east. Snowfall and wind-drifted snow this past week have overloaded these weak layers, with several remotely-triggered avalanches. Today's increased winds and snowfall will only continue to add load and stress to this snowpack.
These recent avalanches - as well as continued loud, booming collapses and cracking - are huge red flags, telling us that the weak snowpack structure still exists and needs more time.
I was on Cutler Ridge on Thursday, and talk about the poor snowpack structure that exists.
Avoid slopes steeper than 30° on mid and upper elevation aspects facing west, through north, and east. Triggering an avalanche on these slopes is likely; they may be up to 2' deep and several hundred feet wide.