Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 2–3
2 to 4 ft foot slabs formed from the end of January storms rest on top of several faceted weak layers and depth hoar near the ground. Although it's been a week since the last significant loading event, strong west winds have been creating stiffer slabs on the surface and are slowly loading slopes that hang delicately in the balance. A couple of natural avalanches from 4 or 5 days ago near and above treeline speak to how fragile the deeper faceted weak layers continue to be. These were large to very large avalanches and would've been unsurvivable. Below treeline, these persistent slab avalanches may be smaller but could have serious consequences if they take you over a cliff or bury you in a terrain trap.
Obvious signs of instability like shooting cracks and loud audible collapses may not be present in travels. Taking the time to dig down deeper into the snowpack is the only way to assess whether this strong over weak snowpack structure exists. To mitigate the hazard, avoid being on or connected to slopes steeper than 35 degrees as you may be able to trigger an avalanche from below and these avalanches may run long distances.
Large natural avalanche on a cross-loaded west gully near treeline. The avalanche failed on facets 2 to 5 feet down in the snowpack.