Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
Dangerous avalanche conditions exist on some slopes facing northwest through north and east at all elevations. Avalanches are failing on a layer of faceted snow (a persistent weak layer, or PWL) that formed during the January/February drought. Avalanches failing on this PWL are 1-3' deep and over 100' wide. Friday's snowmobiler-triggered slide in Farmington Canyon provides an example of this avalanche problem (photo below).
I traveled to Ben Lomond on Sunday and found this poor structure of a stronger slab on top of weaker snow and my partners and I kept to lower-angled slopes.
A few additional notes of caution:
- Signs of instability may not always be present: you may or may not see or experience shooting cracks or audible collapsing.
- Tracks on the slope offer zero signs of stability. Avalanches can take out multiple existing tracks.
- You can trigger these avalanches remotely - from a distance or from below.
The good news is that Sunday's dense snow will provide safer and superb riding conditions on lower-angled slopes with nothing steeper above you.