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Avalanche Forecast

Archived

Feb 11th, 2026–Feb 14th, 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

Waterton Lakes, Waterton.

As temperatures continue to drop, so has the avalanche hazard.

Skiing holds a mix of firm and crusty surface conditions with the occasional pocket of wind effected snow from the latest snowfall.

Confidence

Avalanche Summary

Isolated loose wet avalanches (up to size 1) observed from the latest warming event.

Snowpack Summary

Alpine/Treeline: 5 cm of recent snowfall has been redistributed by moderate westerly wind. This sits on a widespread melt freeze crust over moist snow. The mid and lower snowpack consist of several crusts and faceted layers and is well settled. Total snow height is 160-200cm.

Below Treeline: 2-5 cm of recent snowfall sits on a crust. Underlying layers are moist to ground. Total height of snow is 30-100 cm.

Weather Summary

Thursday

Partially cloudy with an alpine high of -3 °C. No precipitation expected and winds 20km/h SW

Friday

Mix of sun and cloud with an alpine high of -4°C. No precipitation expected and winds will be gusting 55km/h SW

Saturday

Mix of sun and cloud with some flurries expected. Alpine high of -4°C with winds gusting 55km/h

Current weather forecast: Mountain Weather Forecast

Weather tables found here.

Terrain and Travel Advice

  • Approach lee and cross-loaded slopes with caution.
  • A hard crust on the snow surface will help strengthen the snowpack, but may cause tough travel conditions.

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.