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Avalanche Forecast

Archived

Jan 24th, 2026–Jan 25th, 2026

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.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Microwave-Sinclair, North Bulkley, South Bulkley, Telkwa.

Crusty conditions prevail once again.

Confidence

High

  • We are confident due to a stable weather pattern.

Avalanche Summary

January 22 to 24

  • No new avalanches reported but observations are limited. Consider submitting a report to the MIN if you are out in the mountains.

January 21

  • There was a report of a cornice fall that had likely failed during the previous afternoon in the heat of the day.

January 16-20

  • No new avalanches reported.

Snowpack Summary

The snow surface is highly wind-affected in exposed alpine terrain.

Below approximately 1600 m, the surface crust is up to 20 cm thick and poses additional slip-and-fall hazards. Large surface hoar is noted on this crust at treeline and below treeline.

A layer of facets is buried around 50 to 100 cm deep and is slowly gaining strength.

The mid and lower snowpack have no layers of concern. Snowpack depths are generally around 150-200 cm deep at treeline.

Weather Summary

Saturday Night
Clear skies. 30 km/h west ridgetop wind. Treeline temperature -2 °C.

Sunday
Mostly sunny. 40 km/h west ridgetop wind. Treeline temperature -3 °C.

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

Tuesday
Mostly cloudy. 1 to 2 cm of snow. 50 km.h southwest 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.
  • Avalanche activity is unlikely when a thick melt-freeze crust is present on the snow surface.