Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 4
Here's the setup-
A persistent weak layer (PWL) of faceted, old, sugary snow near the ground is found mostly in mid and upper elevation terrain facing the north half of the compass. Late December storms stacked up remarkable amounts of dense, heavy, water laden snow, coupled with very strong winds, bringing the weak layer to its tipping point. And while all of the snow since Christmas is a good thing that eventually heals this weak layer, it doesn't happen overnight. In fact, we've been seeing very large, hard slab avalanches breaking on our early season problem child or, in snow-geek-speak... persistent weak layer (PWL). Wednesday's heavy load of snow, water, and wind stressed this layer again, and I'd continue steering clear of any steep, wind drifted slope, especially those that harbor old October snow.
For now what makes this layer dangerous is:
- Once triggered, avalanches may break hundreds of feet wide.
- Avalanches will be 3-5 feet deep.
- It may not be the first person on a slope that triggers A LARGE, DANGEROUS avalanche, it may be the second, third, fourth, etc. who triggers it.
- Seeing tracks on a slope DOES NOT mean it's safe.
Here's the good news - This layer doesn't exist on south facing slopes which have excellent coverage, and soft creamy powder.
Photo - Northeast facing slope at 9600 feet showing the weak snow near the ground which looks sugary and granular.
Photo - An example of the snowpack on an east facing slope that doesn't have the weak layer. The snowpack is just strong and right-side-up, meaning it's hard at the ground and gets softer near the top. Low elevation east facing slopes generally don't have the weak layer however we have been finding it on east aspects as you gain elevation.