Bollettino valanghe

Snake River Range

Bridger-Teton Avalanche Center
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Pericolo valanghe

Wed
Alta quota
1 · Debole
Limite del bosco
1 · Debole
Sotto il limite
1 · Debole
Non aggiornato — questo bollettino è scaduto 2 years ago. Stai vedendo condizioni passate, non il bollettino in corso.

In sintesi

You may be able to trigger avalanches where the wind has drifted snow and built stiff slabs, and loose snow avalanches are possible on very steep slopes as the day warms up. While small, either of these could be enough to knock you off your skis or sled and send you downslope. Generally stable avalanche conditions exist, and large avalanches on deeper layers are unlikely. 

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely
    Dimensione
    1.5–2.5

    Weak layers of snow are buried 2-4 feet deep on middle and upper-elevation shady slopes. Larger triggers, such as groups, snowmobiles, or falling cornices, will increase the odds of impacting these weak layers. Choosing terrain that minimizes consequences and remaining vigilant if traveling in complex avalanche terrain continues to be a good call. This problem is most commonly found on slopes with the following characteristics:

    • Very steep: slopes steeper than about 35 degrees.
    • Rocky: slopes with variable snow cover due to the roughness of the terrain.
    • Wind-affected: slopes where winds produce variable snow depths.

    ADDITIONAL DISCUSSION

    The above slopes are conveniently also where you are most likely to find:

    • Loose Snow Avalanches: these may be encountered if you are playing in sunny, steep, rocky terrain. As temperatures climb above freezing, it will be possible to trigger loose snow slides large enough to knock you off of your feet. Though they start small, these avalanches can entrain more snow as they travel downslope.  
    • Isolated Wind Slabs: a few stubborn slabs of new snow may remain in very steep (>35°), wind-loaded starting zones above 9,000’. Easterly winds are an unusual wind direction that may have formed slabs in terrain that does not typically see loading. These slabs may also become more sensitive as the day warms up. 

     

Avalanche Discussion

While larger avalanches are unlikely in this zone, the above problems are things to remember as you travel in the mountains today. Encountering these isolated hazards in the wrong terrain can have high consequences. 

Please continue to send us your observations. Thank you!

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