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Avalanche Forecast

Archived

Feb 14th, 2026–Feb 15th, 2026

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

Coquihalla, Harrison-Fraser, Manning, Skagit.

Continually assess conditions as you move through terrain.

Wind slabs could exist on high north facing terrain and wet loose avalanches could be triggered on steep, sunny slopes.

Confidence

Moderate

  • We are uncertain due to a limited number of field observations.

Avalanche Summary

No new avalanches have been reported in this region but observations have been limited.

Snowpack Summary

20 to 40 cm of recent storm snow, that was accompanied by moderate southwest wind, overlies the early February crust/facet layer.

A widespread crust and facet layer from late January is buried 30 to 60 cm deep.

The mid and lower snowpack is generally well settled and strong.

Weather Summary

Saturday Night
Clear skies. 10 km/h southeast ridgetop wind. Treeline temperature -8 °C.

Sunday
Mostly sunny. 20 km/h southwest ridgetop wind. Treeline temperature -7 °C.

Monday
Mostly cloudy. 2 cm of snow. 20 km/h southwest ridgetop wind. Treeline temperature -7 °C.

Tuesday
Mix of sun and clouds. 2 to 5 cm of snow. 20 km/h southeast ridgetop wind. Treeline temperature -7 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be careful with wind-loaded pockets, especially near ridge crests and rollovers.
  • Be alert to conditions that change with aspect and elevation.
  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.