Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Triggering avalanches 1-3' deep on steep slopes facing northwest through north and east at all elevations remains possible. These avalanches are failing on a persistent weak layer (PWL) that formed during the January/February drought. Plenty of local observers have found this layer in the Ogden mountains.
Many of these avalanches are being triggered at the mid-elevations and often in slight openings in otherwise dense trees. We've had many close calls throughout March on this weak layer and it's not time to let our guard down. Travel advice: Where the faceted snow is buried choose slopes less than 30° in steepness, with no overhead hazard.
A few things to remember when dealing with these persistent weak layers:
- You won't know exactly when and where you will trigger the avalanche, but you will probably trigger it from a distance. These types of avalanches are unmanageable.
- Tracks on the slope offer zero signs of stability. Avalanches can take out multiple existing tracks.
- If you do choose to ride slopes where this layer exists, stack the odds in your favor by choosing slopes with a clean runout zone free of trees and rocks that would cause trauma if you do trigger an avalanche.
Photo of the poor snowpack structure from Drew's field day yesterday in the Three Temptations.