Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 2–3
While triggering a deep persistent slab avalanche is unlikely, this problem is lingering. Here are a few scenarios to consider when planning your day in the mountains:
- Old October snow near the ground: These grey, crumbly facets are now buried 4-6 feet deep on most slopes. This layer has plagued us all season and is now less worrisome, but it is keeping avalanche professionals leery of very steep alpine terrain.
- Crust + facets below the recent storm snow: This less obvious layer may exist on very steep (35-45*) slopes facing SW-S-SE. Several 2-3 foot thick, natural avalanches failed on this layer during the last storm.
- Abnormally large cornices and wind features on exposed ridges: Cornices are much larger than normal for this time of year—think school bus-sized— and some could be sensitive to your weight. Cascading down a steep, rocky slope with large cornice chunks would be dangerous on its own, and it could trigger a sizeable avalanche on the slope below.
Where are you most likely to trigger avalanches today? Where you can check most of these boxes:
- "Prime time" slope angles around 35-45* in steepness
- Wind-loaded slopes, or slopes where wind created hard or stiff layers in the upper snowpack
- Rocky slopes with variable snowpack depths—its easier to trigger avalanches in places where the weak layer is 1-3 feet below the surface
Avoid terrain where you check all of the boxes above (photo to right) to reduce the chances of triggering large avalanches.
This large, natural avalanche released naturally near the end of the last storm in very steep, rocky, wind-loaded upper elevation terrain in the 4th of July drainage in the White Cloud Mountains.