Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 2
Our area continues to be plagued by a layer of faceted snow—in this zone, it's buried beneath a dense 1.5-2' 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. Now that we've gone more than a week without significant loading, we know the stability is improving—but it's difficult to say by how much. Reports of snowpack collapsing yesterday on Galena Summit and Horton Peak are signs that triggering an avalanche is most definitely still on the table.
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.
(1/19/2021) Large persistent slab avalanche that failed in the White Clouds around our last storm on January 13th.