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Avalanche Forecast

Archived

Feb 16th, 2026–Feb 17th, 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

South Coast Inland, Birkenhead, Duffey, South Chilcotin, Stein, Taseko.

Carefully assess steep terrain for wind slab before committing.

Small, isolated wind slabs may linger at treeline and above.

Confidence

Moderate

  • We are uncertain due to the variability of wind effect on the snowpack.

Avalanche Summary

Over the past couple days several, small  wind slab and dry loose avalanches have been observed in the region. These avalanches were triggered naturally and by skiers in steep terrain.

Snowpack Summary

10 to 20 cm of recent snow with moderate to strong southwest wind has formed deeper deposits on leeward slopes but may have scoured the surface back to a crust on windward terrain and ridge tops. This new snow overlies a layer of surface hoar on sheltered features.

20 to 40 cm sits over the early February crust that is thin and breakable on northerly aspects to ~2300 m and thick on southerly aspects.

A widespread crust and facet layer from late January is buried 40 to 100 cm deep.

The mid and lower snowpack is generally well settled and strong. Snowpack depth at treeline is around 150 cm.

Weather Summary

Monday Night
Mostly cloudy. 3 to 4 cm of snow. 20 km/h south ridgetop wind. Treeline temperature -9 °C.

Tuesday
Mix of sun and clouds. 1 cm of snow. 10 km/h east ridgetop wind. Treeline temperature -11 °C.

Wednesday
Mix of sun and clouds. 10 km/h southwest ridgetop wind. Treeline temperature -15 °C.

Thursday
Mostly sunny. 10 km/h northwest ridgetop wind. Treeline temperature -16 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be alert to conditions that change with elevation, aspect, and exposure to wind.
  • Pay attention to isolated wind affected features in the alpine, as well as cross-loaded features at treeline.
  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.
  • Pay attention to cornices and give them a wide berth when traveling on or below ridges.

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.