Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2
A poor snow structure with a persistent weak layer (PWL) of faceted snow exists on shady slopes at mid and upper elevations. It'll be along the higher elevation wind drifted terrain where it is possible to trigger an avalanche 1-3 feet deep and over 100 feet wide. Signs of instability such as cracking and collapsing are more obvious at mid-elevation slopes out of the wind zone.
I am uncertain if the incoming storm will tip the scales of our PWL, but I am certain every slope holding weak snow has a tipping point. Be observant and cautious as the incoming storm adds load to our weak structure.
Photo: Drew Hardesty's snowpit below highlighting our current weak structure.