Boletín de aludes

Chic-Choc Mountains

Jan 19 – 20, 2025Avalanche Canada
Ver en el mapa
Archivado · caducó 2 years ago

Peligro de aludes

Tue
Wed
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil

Lo esencial

Wind slabs are still reactive and can be triggered remotely.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely
    Tamaño
    1–2

    New wind slabs are forming on the eastern and southern slopes. The wind slabs are hard, and therefore a little more difficult to trigger, but they promote good propagation. They rest on fragile layers that were already reactive in our tests.

Confidence

Moderate

Avalanche Summary

A size 2 avalanche has been reported. The avalanche occurred on the morning of January 19 in Mines Madeleine, on an eastern slope at tree line. The avalanche was remote-triggered from the ridge. The crown was approximately 30 to 50 cm thick.

If you head into the backcountry, thanks for sharing your observations on the Mountain Information Network (MIN).

Snowpack Summary

At treeline and in the alpine, the surface snow is affected by the wind. Inside the snowpack, there's a thin layer of frost about 20 cm deep, a layer of facets at about 40 cm and a refreezing crust at 60 cm. These layers are reactive in our tests and could be triggered by a smaller surface avalanche. The average snowpack thickness varies between 90 and 120 cm.

Weather Summary

WEATHER FOR THE CHIC-CHOCS RIDGES AND SUMMITS

Sunday evening and night: Snow. Accumulation of 2 cm. North wind 20 km/h. Low -14.

Monday: Snow, accumulation 2 to 4 cm. Wind northwest, 40 to 50 km/h. Temperature dropping to -20.

Tuesday: Mostly sunny. Wind west, 30 to 40 km/h. High -25.

Wednesday: Sunny. Wind northwest, 40 to 50 km/h. High -25.

For more details, see the Chic-Chocs alpine weather forecast.

Terrain and Travel Advice

  • Wind slabs are most reactive during their formation.
  • Be aware of the potential for large avalanches due to buried weak layers.

Regiones cubiertas