Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1.5–2.5
We received reports of a handful ofhuman-triggered avalanches over the weekend. Many of these were remote triggers, failed on the weak sugary facets buried ~2 ft down and are clear indicators that the January drought layers are still a threat. Triggering similar avalanches today is most likely in recently wind-loaded terrain. Persistent Slabs can release in surprising ways. They can be much wider than expected and be triggered remotely—from flat terrain below, above, and to the sides of steep slopes.
Last week's storm snow buried weak facets, surface hoar, and crust-facet combinations on many middle and upper-elevation slopes. More deeply buried weak layers that formed during the extended Jan-Feb drought (facets, crust + facets, surface hoar) have not healed and remain suspect, primarily on NW-N-NE-E aspects above and below the middle-to-upper elevation transition.
Avoiding steep, wind-loaded slopes is the best way to avoid trouble today. Please remember that avalanches are also possible in more sheltered terrain. Snowpack cracking and collapsing are clear signs of unstable conditions.
(2/19/2026)
Very large avalanche on McDonald Peak in the southern Sawtooths. NE @ 9,500'.
Photo: Sawtooth Avalanche Center