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Avalanche Forecast

Archived

Mar 10th, 2025–Mar 13th, 2025

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

Regions

Waterton Lakes, Waterton.

The potential remains for triggering a persistent slab avalanche in northerly alpine terrain, where the new crust does not cap the weak layer.

With windy conditions at upper elevations, be cautious of newly formed slabs in steep wind-affected areas. The best skiing will likely be found in sheltered terrain at or below treeline.

Confidence

Moderate

Avalanche Summary

No new avalanches observed.

Snowpack Summary

5–10 cm of new snow rests on wind slabs up to 20 cm deep in open, wind-affected areas and on a crust 5 -30 cm thick everywhere else except for sheltered north-facing slopes. The January drought layer lies 40–100 cm deep, with snow depths at treeline averaging 130–200 cm.

Weather Summary

Temperatures will remain below zero degrees at treeline and above throughout the forecast period. Expect intermittent snowfall and windy conditions, especially in the alpine. See the table below for detailed forecasts.

Check out the Mountain Weather Forecast for the most up to date information.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind-affected terrain.
  • Avoid thin areas like rocky outcrops where you're most likely to trigger avalanches on deep weak layers.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.