Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 1–2
Triggering avalanches that break on facets above a crust or buried surface hoar remains a concerning possibility in the mountains of the East South. Tuesday brought another round of natural and remotely triggered avalanches up to D2 failing on buried surface hoar just over the ridge at Crystal Mountain. Other backcountry travelers traveling near Crystal also reported a handful of whumphs and long shooting cracks with the same weak layer as the culprit. This bullseye information is hard to overlook, especially when we know the structure is widespread across the region.
Wind loaded slopes have the potential to produce the largest avalanches, but any steep slope should be considered suspect during periods like this. Since these weak layers aren’t too deep yet, you can still use hand pits and snowpack tests to easily locate these layers and check for reactivity. However, digging down can only prove a weak layer's presence, not its absence. They shouldn’t be used to determine if a slope is safe.
There have been several close calls across the region this past week. Don’t add to the tally. You can significantly reduce your exposure to this problem by staying off steep, open slopes - especially where the wind has drifted snow into stiffer slabs.
(2/24/2026)
The 2/13 interface is easy to spot with a clean pit wall. It's a thin grey line a few inches above the prominent 2/7 crust.
Photo: Dallas Glass