Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 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 except those facing south. Snowfall and wind-drifted snow this past week have overloaded these weak layers, with several remotely-triggered avalanches. Wednesday's remotely-triggered slide in Dry Fork in American Fork canyon got my attention as it was triggered from tracks on an adjacent, low-angled slope and pulled out a 2' deep hard slab that ran through trees. Thursday's remote slide in Banana Days and then sympathetically-released slide in adjacent Main Days illustrates how strong and connected the slab on top of the PWL has become. This is likely a good proxy for the Provo-area mountains.
This video provides a good overview of the snowpack in the Provo-area mountains:
These recent avalanches - as well as continued loud, booming collapses and cracking - is the snowpack talking to us, and the message isn't Happy Holidays.
Avoid slopes steeper than 30° on 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.
The good news is that low-angled slopes in non-avalanche terrain are riding quite well!