Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Our area continues to be plagued by a layer of faceted snow—in this zone, it's buried beneath a 1-2' thick slab. Since it was first buried in December, we've recorded nearly 400 avalanches—the vast majority broke on this persistent weak layer. Around 20 of these were human-caused. To say this layer has a poor track record is a bit of an understatement.
Two factors make this persistent slab problem particularly long-lasting: 1) The layer is especially "bad" since it formed during 3-4 weeks of perfect faceting conditions, and 2) It was slowly loaded over the course of a month by a series of small to medium storms. Snowfall in this zone has heavily favored the Soldiers and the Smoky Mountain Crest near the head of Warm Springs. In these areas, the weak facet layer is capped with a dense slab on many slopes—a recipe that's proven dangerous time and time again. Closer to the Wood River Valley, this slab is less common and more closely tied to areas with wind-drifted snow.
You can reduce your risk by avoiding slopes over about 35 degrees, especially those that have been affected by the wind. Pay attention to what's below you—look for trees, rocks, gullies, and other terrain traps. Given the possibility of remote-triggering slides, avoid terrain with steep slopes above you.