Avalanche forecast

Galena Summit & Eastern Mtns

Sawtooth Avalanche Center
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Avalanche danger

Fri
Alpine
3 · Considerable
Treeline
3 · Considerable
Below
2 · Moderate
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Highlights

You’re most likely to trigger a large, thick avalanche on steep slopes facing the northern two-thirds of the compass, where the wind frequently blows, or the snowpack depth is variable. Expect wet snow avalanches in very steep, rocky terrain receiving direct sun. Cornices are large and may be unstable—give them a wide berth.

Avalanche problems

  • Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    2–2.5

    Slabs exist above widespread, weak layers (facets, surface hoar, crusts, and combinations). Persistent Slab avalanches are most likely in the thinner snowpacks of the Pioneer and Boulder Mtns in the southeastern part of this zone. Before triggering an avalanche, you're unlikely to experience obvious signs of instability like snowpack cracking and collapsing or whumpfing. Persistent Slabs can release in surprising ways and break much wider than expected. You are most likely to trigger a dense, 2-4 foot thick avalanche where:

    • The snowpack is less than 4 feet thick—relatively shallower spots may exist where the wind frequently blows, and the slab is not uniformly thick.
    • Any part of the slope you are on or connected to is steeper than about 35 degrees
    • The slope faces the northern 2/3 of the compass
    • A smaller wind slab or loose snow avalanche overloads the buried weak layers

    Additional Discussion - Wind Slabs: You may find sensitive wind slabs near ridgelines and along steep mid-slope gullies. You can reduce your chances of triggering a wind slab by avoiding slopes with obvious signs of wind-loading, such as new cornice growth and large dunes or pillows of wind-blown snow. Cornices are large and may be unstable. Warming temperatures may cause overhanging cornices to sag and fail. Limit time beneath these features and give them a wide berth when traveling along ridges. 

    (2/26/2025) Large slab avalanche on Boulder Peak, Boulder Mountains. SE @ 10,000'. Photo: Sawtooth Avalanche Center

  • Loose Wet

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Likely
    Size
    1.5–2

    Loose snow avalanches are likely on very steep, rocky slopes receiving direct sun. These slides often initiate near the base of trees and rocks, gathering snow and growing in size as they move downhill. Rollerballs, or pinwheels, signify that the snow is heating up, and wet avalanches may soon follow. 

    While most will start small, they may will grow large and dangerous or push you into unwanted terrain. Some slides have the potential to flank out into wider wet slab avalanches. Even small slides are consequential above terrain traps such as gullies, creeks, and thick timber. Plan your day to avoid lingering under steep, sunny slopes when the sun is out.

    (2/26/2025) Small natural wet loose avalanches in the Boulder Mountains. Photo: Sawtooth Avalanche Center

Avalanche Discussion

Persistent slabs top the problem list. We've observed a couple of very large slab avalanches in the Boulder Mountains that we estimate released during recent intense wind-loading. Based on the depth and aspect of the slides, it's likely that these slabs released on a combination of crusts and facets. While adding stress to buried weak layers, wind-loading also built large, sensitive cornices and drifts that remain a concern today.

It's day 2 in a string of warm, sunny days. Last night, temperature inversions kept upper elevations warmer than lower elevations and will be ahead of the curve today as surfaces soften. Today's sunshine will have to overcome crusts at the surface, but alpine temperatures in the 40s F and strong sunshine will eventually turn the surface to mush. This zone has an abundance of craggy, sheltered cirques, perfect for producing large wet avalanches. Steep, sunny slopes are riddled with crust/facet layers. As meltwater moves deeper into the snowpack, we may see large, destructive wet slab avalanches.

Wet snow will slide far and fast on these crusts beneath the surface. The timing of wet snow avalanche problems varies greatly with location, aspect, and elevation and is nearly impossible to predict. Build this uncertainty into your travel plans and limit time on or under steep, sun-drenched slopes. 

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