Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–2.5
This zone has persistent weak layers buried 3-5 feet deep on most middle and upper elevation slopes on the north half of the compass. Feedback in the form of avalanches on these layers has been rare and unreliable but recent large avalanches, such as the cornice fall yesterday at Targhee and the very large avalanche last Saturday on No Name Peak, make it clear that these layers are still a potential problem. Look for clues to help you avoid the thin spots where your weight could trigger a weak layer. Spending time beneath a corniced ridge is also not a good idea. You can further reduce your exposure to this problem type by:
- Choosing moderate slopes with low consequences. Safer travel options always exist by sticking to slopes less than ~30 degrees.
- Avoiding shallow areas. The weak layer is more easily triggered where it is closer to the surface. The thinner edges of slabs are often the trigger point for much thicker slabs.
- Avoiding terrain where wind slabs sit on persistent weak layers. Triggering a wind slab or cornice significantly increases your objective hazard and will more easily impact deeper layers.
(2/17/2024) Photo: Teton County SAR
The avalanche on No Name peak is a reminder of the destructive power of an avalanche failing on a deeper weak layer. This one required a very large trigger - either a cornice fall or possibly a smaller avalanche. Steep, rocky terrain like this is a breeding ground for this type of avalanche.