Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
A hepcat with more than nine lives up his sleeve, local snowpro extraordinaire Trevor Katz remotely triggered this hard slab yesterday on a steep, rocky, shady slope in Upper Weber Canyon.
It is a tricky game right now as rotten November snow turned persistent weak layer sits beneath a strong, dense, cohesive slab that developed from several storms worth of snow, coupled with strong winds. On mid and upper elevation slopes, especially those in the windzone facing the north half of the compass, recently triggered avalanches are breaking 1-3 feet deep, failing on old snow near the ground. Steep, rocky slopes with a thin, shallow snowpack are at the center of the bullseye terrain and need to be avoided.
Here's the challenge... in wind-sheltered, mid-elevation terrain, the slab is softer, not quite as reactive, and we're seeing fewer red flags. But let's not take our eyes off the prize... it's still a strong snow over weak snow setup and that structure is always a big, red flag.
Remember, we can trigger persistent slab avalanches remotely or from a distance. Once initiated, today's avalanches may break deeper and wider than we expect, taking us for a body-bruising ride, raking us through rocks, trees, stumps, or deadfall.
Red flags are keeping us on our toes on the north half of the compass and can't be ignored. All the snowpros I knows are observing no shortage of audible collapses and cracks shooting out hundreds of feet around them.