Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Very Likely
- Größe
- 2–3.5
When you head into the mountains today you will be dealing with a wintertime snowpack harboring the types of weak layers that we are used to dealing with in January and February (watch this video). We have two sets of weak layers that we are worried about, you can clearly see them both in the photo at right/above.
- March Weak Layers: Storms over the past 10 days built a 2-3+ foot thick slab on top of layers of weak snow formed earlier this month. Based on limited observations, these layers appear to be at their worst on slopes that face the sun, where crust+facet combinations exist. The slab over this weak snow is thick enough that avalanches failing on it are possible even in sheltered terrain.
- February Weak Layers: A very dense, 3-6 foot thick slab of snow is uncomfortably resting on weak snow underneath. This combination was responsible for two historic natural avalanche cycles in mid-March. Very large natural avalanches failed on all aspects of the compass. The most recent triggered avalanche involving this snow occurred Friday in the Frenchman's drainage near Smiley Creek when riders remotely triggered a slide that broke 4-5 feet deep and 800+ feet wide (photo at right/above). The riders were at least 500 feet away on the ridgeline above when they triggered the slide. Blocks of snow the size of small cars remained intact as they traveled downslope, breaking green trees along the way. Triggering an avalanche involving this deeper weak layer is less likely than a slide higher in the snowpack, but the consequences would be devastating.
Yesterday's big storm and today's ongoing snowfall and wind loading are adding significant stress to these layers. Persistent slabs are challenging beasts to deal with. You can trigger them from long distances away from where the avalanche releases. Slides may break much wider and deeper than you expect, wrapping around large terrain features. Tracks on a slope are not an indicator of stability, these slides can fail after many skiers or riders have traversed a slope. Smaller avalanches can be effective triggers for these deeper weak layers as they travel downslope.
(3/31/2023)
Crown of a very large avalanche that was remotely triggered by riders from at least 500 feet away on the ridgeline above. It broke 4-5 feet deep and 800+feet wide. This slope faces W at 9,300' in the Frencman's drainage near Smiley Creek. You can clearly see the two sets of persistent weak layers in our snowpack in this photo.