Bollettino valanghe

Snake River Range

Bridger-Teton Avalanche Center
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Pericolo valanghe

Sun
Alta quota
2 · Moderato
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

New snow and wind have formed sensitive wind slabs up to 1 foot thick at upper elevations. Pay attention to signs of wind-loading including the formation of pillows and shooting cracks. It is unlikely you will trigger a large avalanche failing on buried weak layers near the ground.

 

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–1.5

    Wind slabs up to 1 foot thick have formed in the upper elevations after a storm system brought 2 to 4 inches of new snow and moderate winds from the north. Expect to find these generally small slabs on all aspects as winds have shifted from the north to the east overnight. Before the most recent storm, snow surfaces weakened over the last two weeks. New wind slab formations on this surface will be sensitive and human triggers are likely.  Recently, multiple small wind slabs have failed on this weak snow demonstrating the poor structure beneath the new snow. Expect to find these slabs along ridgelines, in cross-loaded gullies, and on steep convex rollovers. Pay attention to signs of wind-loading including the formations of pillows, textured surfaces, or shooting cracks. Triggering a small wind slab can have large consequences, especially near gullies, cliff bands, and trees. Moving to terrain sheltered from the wind will help you avoid this problem.

    A shooting crack observed in a hollow sounding wind textured pillow.

    Photo: Bridger-Teton Avalanche Center

  • Persistent Slabs

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

    Triggering a large hard slab avalanche is unlikely. Weak layers of snow buried 2-4 feet deep in the Snake River range are adjusting to the weight of the snowpack.  Instability is most likely to be found in very steep, north-facing terrain. Triggering a large avalanche will be most likely in thin rocky areas where you can impact the weak layers.  Larger triggers, such as groups, snowmobiles, or falling cornices, will increase the odds of impacting these weak layers. 

    (1/16/2025)

    An example of complex terrain in the Snake. Very steep, wind affected slopes where trigger points for a hard slab avalanche could be close to the surface.

    Photo: Bridger-Teton Avalanche Center

Avalanche Discussion

Winds have varied from W to N to E over the last 48 hours. As such, wind slabs are expected on all aspects today. The less common eastern wind today will cause wind slabs to form in unusual locations. Stay alert for signs of wind-loading throughout the day as these eastern winds will continue into the evening and overnight. 

We are now two weeks out from an observed avalanche failing on a persistent weak layer. Buried weak snow on the ground still exists but has mostly adjusted to the weight of the current snowpack. It will probably take a significant increase in load, like a big storm, to see any activity on this layer, and even that is hard to predict.

Please continue to send us your observations!

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