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Avalanche Forecast

Archived

Jan 6th, 2026–Jan 7th, 2026

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Chic-Choc Mountains, Chic-Chocs.

In some places, wind slabs may still be reactive.

Confidence

Moderate

  • The snowpack structure is generally well understood.

Avalanche Summary

No new avalanches reported or observed.

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

Snowpack Summary

The surface snow has been heavily affected by westerly winds. In sheltered areas, there is 20 to 30 cm of light snow on the surface. Facets are developing on the December 20 melt freeze crust, which is between 30 and 50 cm deep.

Due to the wind, snow distribution is very uneven in alpine terrain and near treeline: some slopes are almost bare, while others have significant accumulations of wind-blown snow.

The average snow depth at mid-mountain ranges from 60 to 100 cm.

Weather Summary

WEATHER FOR THE CHIC-CHOCS RIDGES AND PEAKS

Temperatures will rise over the next few days.

Tuesday evening and night: Partly cloudy. Wind from the southwest at 10 à 30 km/h. Low -14.

Wednesday: Cloudy. Wind from the south at 20 to 30 km/h. High -3.

Thursday: Cloudy. Accumulation of 1 to 2 cm. Wind from the northwest at less than 15 km/h. High -4.

Friday: Intermittent snow. Wind from the southwest at 20 to 40 km/h. High 0.

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

Terrain and Travel Advice

  • Small avalanches can have serious consequences in extreme terrain. Carefully evaluate your line for slabs before you commit to it.
  • Seek out wind sheltered terrain below treeline where you can avoid wind slabs and find great riding.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.