Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2
What is it? Recent storms have favored this zone and buried newer weak layers consisting of facets or crust+facet combinations in the upper snowpack. These layers are more dangerous where recent winds have added weight to the slab. It's been almost three weeks since the last reported avalanche in this zone that involved buried surface hoar down 1.5-2 feet. It may be getting harder to find the right slope to trigger surface hoar, but it can't be completely ruled out yet.
Where is it? The craggy nature of the Sawtooth Mountains allows recent gusty winds to transport snow to where it piles up below cliffs in alpine bowls (refer to the photo to right/above). These are common locations where slabs can be more sensitive to the weight of a skier or snowmobiler. Buried surface hoar continues to linger in mostly sheltered, shady slopes (facing NW-N-NE). These layers are most likely triggered on slopes steeper than about 35 degrees.
How can you recognize it? Wind-affected slopes will have stiffer snow at the surface, keeping you from sinking deep into the snowpack. You may or may not experience snowpack collapsing and/or cracking while traveling. These red flags are obvious signs of instability. The surface hoar layer is subtle and may not "jump out at you" when searching for it in a snowpit (see photo here).
How can you manage it? You're most likely to trigger persistent slab avalanches involving either the shallowly buried facets/crust+facet combos on slopes steeper than about 35 degrees with stiff wind-blown snow or slabs. You can reduce the chances of tangling with surface hoar-driven avalanches by avoiding very steep (greater than about 35 degrees), shady (facing NW-N-NE) middle elevation slopes.
ADDITIONAL DISCUSSION: Recent moderate to strong NW winds have created dense slabs in exposed middle and upper elevations. You may find wind slabs near ridgelines, on the sides of gullies and chutes. Cracks shooting out from your skis or sled are an obvious sign of instability. Watch for drifts, dunes, and ripples on the snow surface. Wind slabs can have a smooth, chalky appearance and feel and sound hollow, like a drum. The easy move is to avoid obviously wind-loaded slopes steeper than about 35 degrees.
(1/23/2023) A large avalanche released below a cliff band in the Central Sawtooths on a east facing slope at 9600'.