Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
You could trigger a 2-4' thick persistent slab avalanche on buried weak layers (sugary facets or crust + facet combinations). This problem is worst on middle and upper elevation slopes facing W-NW-N-NE-E-SE.
Unfortunately, unstable slopes probably won't provide obvious signs of instability, like snowpack collapsing or cracks shooting out in front of you. Snowpack stability tests are likely to be inconclusive and are of limited use. Tracks on a slope don't mean it's safe. Avalanches can be triggered by the second, third, or fourth rider on a slope. In low probability/high consequence situations like this, there's a good chance the first sign of instability you'll see is the avalanche you trigger.
The likelihood of triggering a slide is not that high, but the thick, dense slab makes the consequences severe. Persistent weak layers can fail unpredictably and break wider and higher on slopes than you might expect. You can reduce, but not eliminate, your risk by avoiding slopes steeper than about 35 degrees—especially large avalanche paths and those with ugly consequences if you are caught in a slide.
ADDITIONAL DISCUSSION: Today's storm may form thin, sensitive slabs of wind drifted snow at upper elevations. These slabs will be more dangerous in the Soldiers where more snow is expected. Look for smooth pillows of windblown snow near ridgelines and mid-slope gullies. Loose snow avalanches are possible during periods of intense snowfall. They may also occur during brief periods of sunshine, especially in very steep, rocky terrain.