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Avalanche Forecast

Archived

Jan 28th, 2026–Jan 29th, 2026

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

Regions

Lizard-Flathead, Akamina, Flathead, Lizard, Moyie, Crowsnest North, Crowsnest South.

Assess steep lines before committing.

Small, isolated wind slabs may be reactive due to the surface hoar beneath them.

Confidence

High

  • We have a good understanding of the snowpack structure and confidence in the weather forecast.

Avalanche Summary

On Monday and Tuesday the recent snow produce sluffing in steep terrain and a few small, isolated wind slabs.

Snowpack Summary

The snow surface is variable. On sheltered features up to 10 cm of recent snow sits over a surface hoar crust combo. In sun exposed terrain a sun crust is likely, on high north facing terrain some dry snow may still be found.

The mid and lower snowpack is well settled.

Check out this MIN from our field team for more info.

Weather Summary

Wednesday Night
Cloudy. 40 km/h west ridgetop wind. Treeline temperature -7 °C.

Thursday
Cloudy. 1 to 2 cm of snow. 50 km/h west ridgetop wind. Treeline temperature -5 °C.

Friday
Cloudy. 1 to 2 cm of snow. 50 km/h west ridgetop wind. Treeline temperature -4 °C.

Saturday
Mix of sun and clouds. 1 to 5 cm of snow. 50 km/h west ridgetop wind. Treeline temperature -3 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • A hard crust on the snow surface will help strengthen the snowpack, but may cause tough travel conditions.
  • Carefully evaluate big and steep terrain features before committing to them.
  • Wind slabs are isolated, but may remain reactive.

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.