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Avalanche Forecast

Archived

Dec 4th, 2025–Dec 7th, 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.

Good Skiing can be found in alpine areas but it comes with a cost. The travel in the lower elevations is a wee bit of a challenge. Watch for pockets of windslabs along ridgelines and crossloaded features.

Confidence

High

Avalanche Summary

No new avalanches or reports today.

Snowpack Summary

Lower elevations are still pretty rugged for travel in most areas. The crust that developed in November though is providing good travel opportunities!

Closer to treeline and above, winds have started to form windslabs on all aspects in immediate lees with the variable directions winds. The bond of the new snow to the rain crust is starting to facet out with the cooler temps, something to continue to monitor as new snow loads on top . The crust starts to disappear at around 2350m so be careful in the higher elevations to not hit rocks or other features if the crust is not present. The height of snow is about 60-100cm on average.

Weather Summary

Mix of sun and cloud with moderate westerly winds. Temperatures near -8C. Trace new snow over the next 24hrs.

https://hpfx.collab.science.gc.ca/~fsg006/productviewer/ab/table/AB_Rockies_Forecast.html

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Wind slabs are isolated, but may remain reactive.

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.