Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
Slabs 1 to 4 feet thick have formed over several persistent weak layers in the snowpack: Weak facets near the ground and surface hoar layers in the upper snowpack. The problem has been most active on northerly and easterly facing slopes, with some avalanches on westerly facing terrain as well. Persistent slabs are gradually becoming more difficult to trigger and signs of instability are becoming less frequent, but if you cross the wrong slope or the wrong spot on a slope, a single collapse can result in a surprisingly large avalanche involving most of the snowpack. Persistent slabs could break wider than you expect, and they can be triggered from flat slopes connected to steeper terrain above you. You can reduce your risk by traveling on slopes where the problem isn't highlighted above, or by traveling on small terrain features without terrain traps. You can avoid the problem on slopes consistently less than 30 degrees.
A natural avalanche on an east-facing slope of Treasury Mtn into North Pole Basin. Debris spilled over and triggered another avalanche on the north-facing slope below the cliffs. Likely ran 12/10.