Bulletin d’avalanche

Soldier & Wood River Valley Mtns

Sawtooth Avalanche Center
Voir sur la carte

Danger d’avalanche

Sat
Alpin
3 · Marqué
Limite forestière
2 · Modéré
Sous la limite
1 · Faible
Open full map
Périmé — ce bulletin a expiré 2 years ago. Vous consultez des conditions passées, pas le bulletin en cours.

Points saillants

You're most likely to trigger a large avalanche in areas where the wind has stiffened the snow surface or built thick drifts. You may be able to trigger these avalanches remotely—from flat terrain below, above, and to the sides of steep slopes. 

Problèmes avalancheux

  • Persistent Slabs

    • Alpin
    • Limite forestière
    • Sous la limite forestière
    Probabilité
    Likely
    Taille
    1.5–2

    Wednesday's W and NW winds caused natural slab avalanches to release near exposed ridgelines. Recently formed 1-4 foot thick slabs sit atop various weak layers (facets, surface hoar, crusts, and crust + facet combinations). 

    The widespread nature of the weak layers means avalanches may be triggered on many aspects. The odds you trigger a slide are greatest where wind formed drifts or stiffened the snow surface. Avalanches are less likely but possible on steep slopes more sheltered from the wind. 

    Signs of recent wind loading include cornices, dunes, or drifts. Snowpack collapsing or whumpfing means you've found a sensitive slab. Persistent Slabs can release in surprising ways, break wider than expected, and release above or hundreds of feet away from where they are triggered. Remotely triggering an avalanche from flat terrain below steep slopes remains a concern. Keep a close eye on your partner and the terrain above you.

    (12/15/2024) The Sun Valley Ski Patrol triggered several 12-18" thick pockets of wind-loaded snow while performing mitigation work before opening ski runs. 

    Photo: Sun Valley Ski Patrol

Avalanche Discussion

Wednesday afternoon and evening, wind speeds blew strong to extreme from the W and NW. An observer in the Western Smokys shared this photo of a natural slab avalanche caused by wind loading, and we observed these avalanches north of Ketchum. An observer on Copper Mountain near Banner Summit shared this great photo of wind-affected snow. The persistent slabs described above have two primary ingredients: buried weak layers and a slab. Put that combination into avalanche terrain, and you've got a problem. Since the end of our recent storm, we've found plenty of weak snow, but some slopes lacked a stiff enough slab. Wednesday's wind event changed that in many areas. 

Today, you can drastically reduce your risk of triggering a large avalanche by looking for and avoiding areas with a stiff slab near the snow's surface. Actively seeking out softer snow is safer and more enjoyable but doesn't completely eliminate your risk. Given the sensitive weak layers we're dealing with even deceptively soft slabs have the potential to release in steep terrain. The consequence of these smaller slides increases on slopes with terrain traps like gullies, cliffs, or thick trees. 

Régions couvertes