Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
While we've had few recent reports of instabilty, I'd still be leery of two kinds of terrain today. One is relatively easy to identify; the second is more subtle and sneakier. Triggered slides above terrain traps can have outsized consequences.
The first is upper-elevation leeward slopes that harbor some slabs of stiff, dense snow that remain sensitive to triggering by a person or snowmachine. The second involves slopes sheltered from the sun and wind where a buried layer of weak surface hoar and facets lurks. It's a distinct grey stripe 8 to 16 inches below the surface in terrain above the rain-snow line from the Dec. 7th storm. Layers like this tend to be spatially variable in strength, and thus unpredictable. People often trigger slabs on these layers mid-slope, at convexities or roll-overs where a slope steepens. These changes in slope angle aren't always obvious from above. Both these hazards are isolated at mid-elevations.
Choose terrain today that minimizes the chances and consequences of a surprise today. Stick to slopes that are unlikely to harbor the 12/7 surface hoar and facets, like south and southwest facing slopes. Avoid slopes where a dense layer of wind-stiffened snow rests on the this layer. Choose terrain with a planar or concave profile and runouts clear of gullies, trees, rocks, or cliffs.
(12/14/2024)
The distinct grey stripe in the snowpit wall is the layer of surface hoar and facets buried 12/7.
Photo: David Steele