Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Human triggered persistent slab avalanches are likely today on middle and upper elevations. Various overlapping buried weak layers, including surface hoar, near surface facets, and depth hoar, exist on all aspects at upper elevation and north through east aspects at mid elevation. We are beginning to get reports of multiple large natural avalanches from the past few days, likely failing on these layers.
It will be possible to remotely trigger an avalanche from above, below, or to the side of slopes.
You can recognize persistent weak layers by digging into the snowpack and looking for a dense slab on top of weak, sugary snow. Buried surface hoar can be more difficult to identify in a snowpit but often appear as a thin horizontal line across the snowpit wall face.
Red flags include wumpfing, collapsing, shooting cracks, and recent avalanches. If you encounter any of these or find a poor snowpack structure of buried weak layers below a slab, stick to slopes under 30 degrees.