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Avalanche Forecast

Archived

Dec 25th, 2025–Dec 26th, 2025

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

Regions

Vancouver Island, East Island, North Island, South Island, West Island.

Watch for wind slabs in steep terrain at upper elevations.

Confidence

Moderate

  • Uncertainty is due to the limited number of field observations.

Avalanche Summary

There were no new avalanches observed on Tuesday or Wednesday.

Backcountry reports are very limited. If you head out, please post any photos or observations to the Mountain Information Network.

Snowpack Summary

Many areas are seeing 90 to over 130 cm of recent snow over a melt-freeze crust, with deeper deposits in wind-loaded terrain at treeline and above.

Early-season hazards remain a concern concealed beneath the new snow and will continue to be as the snowpack settles and becomes more supportive.

Weather Summary

Thursday Night

Mostly cloudy. 10 km/h southwest ridgetop wind. Treeline temperature -3 °C. Freezing level 700 m.

Friday

Mostly cloudy with flurries, accumulation 2-5 cm. 20 km/h northwest ridgetop wind. Treeline temperature -5 °C. Freezing level 500 m.

Saturday

Mostly sunny. 30 km/h northwest ridgetop wind. Treeline temperature -6 °C. Freezing level 200 m.

Sunday

Mostly cloudy. 1 cm of snow. 30 km/h west ridgetop wind. Treeline temperature -4 °C. Freezing level 100 m.



More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be careful as you transition into wind-affected terrain.
  • Back off if you encounter whumpfing, hollow sounds, or shooting cracks.

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.