Persistent Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1.5–2
In the past two weeks, skiers and riders triggered several avalanches involving a layer of surface hoar buried 1.5-2 feet deep. A skier triggered a slide on this layer Sunday in the Salmon River drainage (view report). The surface hoar "problem" remains capable of producing avalanches on some slopes steeper than about 35 degrees.
Buried surface hoar is challenging to deal with. Its patchy distribution means you may find it on one slope but not the next, and it can be hard to identify when searching for it in a snowpit (example). It's often best preserved and more sensitive in small clearings and open, wind-protected terrain on shadier aspects.
You can reduce your risk by avoiding slopes facing NW-N-NE that are steeper than about 35 degrees. Consider the consequences of going for a ride. Even small slides can have bad outcomes if they lead to trees, cliffs, or a creek bed.
ADDITIONAL DISCUSSION: Last weekend's snow and northerly wind formed thin, soft slabs in exposed terrain (Cape Horn Mtn). You could trigger a similar slide today. Look for wind slabs near ridgelines, on the sides of gullies and chutes, and near prominent terrain features. Cracks shooting out from your skis or sled are an obvious sign of instability (example).
(1/23/2023) 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.