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Avalanche Forecast

Archived

Feb 10th, 2025–Feb 11th, 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, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Kananaskis, Bow Valley, Highwood Pass, North 40, Spray - KLakes.

Sheltered areas still offer good skiing. Be mindful of the cold temps. Even a minor injury or equipment problem can turn into a serious emergency at -25c.

Confidence

High

Avalanche Summary

No new avalanches have been reported.

Snowpack Summary

Previous storm snow has settled to between 20 and 30cm at treeline. Expect some recent wind slabs in cross loaded gullies and isolated areas in the alpine. The Jan 30 interface is still a question in terms of location and character. It mostly seems to be either a melt/freeze crust, facet layer, buried wind slab or surface hoar. The midpack is supportive in most places, but in rocky areas it has become very weak and "punchy" while walking/sking.

Weather Summary

Some weather models are calling for a low of -27c by Tuesday morning. See the chart below for more info:

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Carefully evaluate big and steep terrain features before committing to them.
  • Be careful as you transition into wind-affected terrain.
  • Avoid steep terrain that is rocky and thin.

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.