Storm Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 3
More avalanche reports have come in that show that a widespread deep slab avalanche cycle has been occurring throughout the forecast area on NW-N-NE-ENE aspects at all elevations. Many of these deep slabs occurred during or immediately after the storm and released naturally. There have been at least 3 that have been human triggered post storm with 2 occurring on Sunday. Deep slab avalanches continue to be an ongoing avalanche problem today.
The issue is a layer of faceted snow that exists 4 to 8' deep below the snow surface. This can be difficult for a backcountry user to get force down to this weak layer where it is deeply buried. Likely trigger points could be areas where the weak layer is closer to the snow surface like near: rocks, trees, cliffs, convex rollovers, and areas with a shallower snowpack.
All of the deep slab avalanches that have occurred so far have had wide propagation and have been large avalanches (D3 or bigger-large enough to destroy a house and break trees up to taking out large swaths of mature forest). Tracks on a slope will not indicate stability as was shown from Sunday's avalanche at Lost Lake (Carson Pass area) where the slope was tracked out before the avalanche was triggered. These deep slabs have the potential to be remotely triggered as was shown by the Negro Canyon avalanche ( Donner Summit area) where the avalanche occurred 500' away from the trigger point in lower angle terrain with shooting cracks traveling up to 1000' away.
Deep slabs are unpredictable and signs of instability may not be present. The only effective management option is avoidance. Avoid slopes steeper than 30 degrees and slopes connected to steeper terrain on NW-N-NE-E aspects. Good recreation conditions currently exist on Northerly aspects that are below 30 degrees in steepness with no steeper avalanche terrain connected.