Avalanche forecast

Galena Summit & Eastern Mtns

Sawtooth Avalanche Center
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Avalanche danger

Tue
Alpine
3 · Considerable
Treeline
3 · Considerable
Below
3 · Considerable
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Highlights

Dangerous avalanche conditions exist—be careful. You're likely to trigger avalanches big enough to bury people on many sheltered and wind-affected slopes. You could trigger avalanches remotely—from gentler terrain above, below, and to the sides of steep slopes. To reduce your risk, you can stick to lower-angled terrain that is not directly below large avalanche paths. 

The danger will increase this afternoon and evening. See the Forecast Discussion for details.

Avalanche problems

  • Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Likely
    Size
    1.5–3

    The calendar says April, but we're facing mid-winter-style Persistent Slab problems (watch this video). We have two distinct problems to consider:

    1. "Fresh" Slabs: Yesterday, a SAC forecaster remotely triggered an avalanche near Titus Ridge. You could trigger 1-2 foot thick slides on many middle and upper elevation slopes. The new snow that fell over the past several days has formed a soft slab above small facets and crust + facet combinations. Watch for obvious signs of instability like snowpack cracking or collapsing. 
    2. Thicker, Older Slabs: While less likely, the possibility of triggering a massive 3-6 foot thick avalanche remains on the table. These hard slabs also rest on weak facets and crust + facet combinations. The most recent triggered avalanche involving this snow occurred Friday in the Frenchman Ck drainage near Smiley Creek when riders remotely triggered a slide that broke 4-5 feet deep and 800+ feet wide (photo at right/above). The riders were at least 500 feet away on the ridgeline above when they triggered the slide. Blocks of snow the size of small cars remained intact as they traveled downslope, breaking green trees along the way. Triggering an avalanche involving this deeper weak layer is less likely than the thinner "fresh slabs", but the consequences would be devastating. 

    The multiple persistent slab problems are creating variable, spooky avalanche conditions. You may or may not see obvious signs of instability on unstable slopes. You may be able to trigger slides from long distances away. Slides could break much wider than you expect, wrapping around large terrain features. Tracks on a slope are not an indicator of stability Smaller avalanches can be effective triggers for these deeper weak layers as they travel downslope.

    Read the Forecast Discussion below for details on yesterday's bullseye information and observations. 

    (3/31/2023)

    Crown of a very large avalanche that was remotely triggered by riders from at least 500 feet away on the ridgeline above. It broke 4-5 feet deep and 800+feet wide. This slope faces W at 9,300' in the Frencman's drainage near Smiley Creek. You can clearly see the two sets of persistent weak layers in our snowpack in this photo. 

  • Wind Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–2

     You may encounter fresh wind slabs in exposed middle and upper elevation terrain. Slabs will be thicker and more widespread in alpine terrain. Any wind slabs that you encounter may be perched above weak facets and/or crusts, making avalanches easier to trigger and wider than you'd expect. Relatively small wind slabs moving downhill could trigger the larger, more dangerous Persistent Slab avalanches discussed above. 

    Look for wind slabs near ridgelines and on the sides of mid-slope terrain features like gullies and ribs. Surface textures like dunes, ripples, or pillows are clues that the wind has been at work. Cracks shooting out from your skis or machine are clear indicators that you've found an unstable slab. 

Avalanche Discussion

The avalanche danger will increase this afternoon and evening as snowfall and increasing wind stress a snowpack that is already on edge. Natural avalanches will become more likely. Stability could decrease rapidly on some slopes. Be ready to adjust your plans if you're out late in the day.  

A quick recap of some important observations from yesterday:

  • SAC forecasters remotely triggered two avalanches (Banner Summit video, Titus Ridge observation).
  • A regular observer reported multiple, large, natural avalanches released around noon near Copper Mtn on E aspects near 8500'.
  • Several medium-sized avalanches released naturally during the day in the Wood River Valley south of Ketchum. All the slides were in west-facing, wind-loaded avalanche paths that were baking in the afternoon sun.
  • A regular observer reported several impressive recent natural avalanches in the Pioneer Mtns (observation with photos).
  • SAC forecasters saw dozens of recent large natural avalanches, including impressive slides on Galena Peak and farther south in the Boulder Mtns (observation with photos). 

What do we make of that information? It's sketchy out there. Recent avalanches failed on many aspects: very sunny slopes, slopes on the "margins" with partial shade and sun, and shadier aspects. Most of the recent activity appeared to involve persistent weak layers (crusts, crust + facet combinations, facets) in the upper 2 feet of the snowpack, but some slides were over 4 feet thick. Many of the recent slides were in relatively sheltered terrain, and many were over 500' wide. 

What can we do with that information? If you're going to play in avalanche starting zones (slopes steeper than about 30 degrees), recognize there's a decent chance you'll trigger a slide big enough to bury you and an outside chance the slide will be big enough to damage or destroy a house. Consider what's above you if you're sticking to gentler slopes; you could trigger avalanches from flat or mellow terrain below steep avalanche starting zones.  

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