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Avalanche Forecast

Archived

Feb 18th, 2026–Feb 19th, 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

Coquihalla, Manning, Skagit.

Loose avalanches remain possible in steep sheltered terrain.

Confidence

High

  • We are confident due to a stable weather pattern.

Avalanche Summary

A few natural wind slabs were observed in steep, north facing  terrain on Sunday. No other recent avalanches have been observed.

If you are heading into the backcountry, please consider sharing your observations with the Mountain Information Network.

Snowpack Summary

20 to 40 cm of recent storm snow, that was accompanied by light to moderate southwest wind, overlies the early February crust/facet layer. The snow surface may become moist on sun exposed slopes.

Another widespread crust/facet layer from late January is buried 30 to 60 cm deep.

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

In forested areas, a light dusting of new snow overlies hard melt-freeze lumps creating very difficult travel conditions.

Weather Summary

Wednesday Night
Mostly clear. 3 cm of snow. 10 km/h east ridgetop wind. Treeline temperature -14 °C.

Thursday
Mix of sun and clouds 10 km/h southeast ridgetop wind. Treeline temperature -14 °C.

Friday
Mix of sun and clouds. 20 km/h southwest ridgetop wind. Treeline temperature -10 °C.

Saturday
Mix of sun and clouds. 40 km/h south ridgetop wind. Treeline temperature -6 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.
  • Make observations and continually assess conditions as you travel.

Problems

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.