Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1.5–2
Several weak layers are buried in the upper 1.5-2.5 feet of the snowpack. On slopes that face away from the sun, you'll find some surface hoar and facets at these interfaces. On slopes that face the sun, you'll find crusts with some small facets here. These weak layers have had some time to get comfortable with the new load that was added last week and the chances of triggering a slide on them is gradually decreasing but hasn't disappeared completely.
You are most likely to encounter a sensitive slab in terrain steeper than about 35 degrees, particularly where the wind has been building slabs on top of these weak layers. Avalanches failing on persistent weak layers can break well above you on the slope and may break wider than you expect. Many of the avalanches that were triggered in mid-January on the prominent layer of surface hoar failed in terrain sheltered from the wind (photo at right/above). Today, avalanches failing in sheltered terrain are less likely but remain a possibility.
ADDITIONAL DISCUSSION: If you head into exposed upper elevation terrain you may find a batch of small, recent wind slabs (photo here). Look for these along ridgelines and near mid-slope terrain features like ribs and gullies. Cracks shooting out from your machine or skis are clear indicators of an unstable slab. Small slabs that knock you off your feet and send you downslope can have high consequences in the wrong terrain. Smaller triggered wind slabs can be effective triggers for the buried weak layers described above.
(1/23/2023) Persistent slab avalanche apparently triggered by a skier on Banner Summit. Slab depth and terrain characteristics are consistent with early January surface hoar layer. 7250', NNW. The date of this avalanche is uncertain, but likely occurred since Jan 18th. Photo taken Jan 23rd.