Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1.5–2.5
An impressively thick, well-preserved layer of surface hoar was responsible for rider-triggered slides, collapsing, and cracking in the Swan Range last weekend, 1/31 and 2/1. This layer is identified by a grey stripe in pit walls and lies within the top foot or so of the surface in sheltered terrain and around two feet deep on wind-loaded slopes.
The recent heat wave has stiffened surface snow into a cohesive slab on polar aspects and a crust of varying strength on sunny slopes. You may not notice signs of instability, such as cracking or collapsing, before triggering a slide. These can be triggered remotely from flat terrain above, to the side, and below steep slopes.
This is a near-surface problem, and hand pits are a useful tool for confirming the presence of a buried weak layer.
Sticking to a supportable crust will minimize the risk of impacting the weak layer. Choose low-angle slopes that are not connected to steep slopes in areas without a crust.
Wet Loose: Today's forecasted rain may wet previously dry snow, resulting in small wet loose slides. If the freezing line rises higher than expected, this problem will become more widespread.
(1/31/2026)
This is a pile of hard slab debris from a remotely triggered avalanche near Mt Aeneas. We assume this slide failed on a buried layer of surface hoar on a wind-loaded slope.