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Avalanche Forecast

Archived

Feb 7th, 2025–Feb 8th, 2025

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

Regions

Akamina, Crowsnest North, Crowsnest South, Elkford East.

Look for areas that have been sheltered from the wind for the lowest avalanche danger and the softest snow.

Confidence

Moderate

Avalanche Summary

  • Thursday: Southwest of Pincher Creek, a small (size 1), rider triggered slab avalanche was reported in east facing treeline terrain. See the MIN post here for more information.

Ongoing sluffing from steep terrain has been reported throughout the region.

Snowpack Summary

15 to 35 cm of soft snow is on the surface in sheltered terrain, with deeper deposits in wind-loaded areas. Wind has varied in direction, so expect to find wind slabs on all aspects.

The new snow may be bonding poorly to old surfaces, which include melt-freeze crusts on sun-exposed slopes, surface hoar or facets on shaded slopes, and wind-affected snow at higher elevations.

The lower snowpack is strong and bonded.

Weather Summary

Friday Night

Mostly clear. 20 to 50 km/h west ridgetop wind. Treeline temperature -20 °C.

Saturday

Mix of sun and cloud. 20 to 50 km/h west ridgetop wind. Treeline temperature -13 °C.

Sunday

Partly cloudy with up to 3 cm of snow. 10 to 30 km/h west ridgetop wind. Treeline temperature -13 °C.

Monday

Mostly sunny. 10 to 30 km/h northeast ridgetop wind. Treeline temperature -20 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid freshly wind-loaded terrain features.
  • 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.