Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Snowfall and windloading this week are forming slabs over the fragile facets and faceted crusts that formed during our long drought. Anticipate unusual and challenging behavior associated with these recently buried persistent weak layers, such as remote triggering and surprisingly wide propagation. Even relatively thin slabs can grow to large sizes on the north half of the compass where they entrain the old, weak snow below (See video). Shooting cracks and collapsing are clear warning signs of the problem. There is isolated potential for slabs in the upper snowpack to step down into older weak layers near the ground, producing a deeper and larger avalanche. You can reliably avoid today's problems by traveling on slope angles that are consistently less than 30 degrees in steepness without overhead hazards.
This photo illustrates the remote triggering potential for avalanches that fail on weak facets or faceted crusts.