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Avalanche Forecast

Archived

Feb 9th, 2025–Feb 10th, 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

Lizard-Flathead, South Rockies, Flathead, Lizard, Bull, Elkford West.

A weak layer of snow is buried 50 to 70 cm deep and is still showing signs of instability.

Large alpine and treeline slopes are still a concern.

Confidence

Moderate

Avalanche Summary

  • Saturday: No new avalanches have been reported though, signs of instability continue to be reported in the region,check out this MIN.

  • Friday : A large (size 2) remote triggered avalanche was reported at treeline on a south aspect on a 35 degree slope. A few small wind slab avalanches were reported on east aspects.

  • Thursday: A few large (size 2 to 2.5) natural avalanches were reported on a southeast and east aspects in the alpine.

Snowpack Summary

A dusting of snow now rests above 35 to 50 cm of soft snow, with deeper deposits in wind-loaded areas. Cold temperatures have kept the recent storm snow loose and low density.

Variable wind speeds and directions through the storm and after mean that the extent of wind-affected snow at different aspects and elevations will vary across the region.

The recent snow has not bonded well to the late January drought layer, which includes melt-freeze crusts on sun-exposed slopes, large surface hoar or facets in sheltered areas, and wind-affected snow in exposed terrain at ridgelines.

The lower snowpack is strong and bonded.

Weather Summary

Sunday Night

Partly cloudy with flurries. 20 to 40 km/h northeast ridgetop wind. Treeline temperature -23 °C.

Monday

Sunny. 10 to 20 km/h north ridgetop wind. Treeline temperature -16 °C.

Tuesday

Mostly sunny. 10 to 30 km/h northwest ridgetop wind. Treeline temperature -14 °C.

Wednesday

Mostly sunny. 10 to 30 km/h northwest ridgetop wind. Treeline temperature -15 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Keep in mind that human triggering may persist as natural avalanches taper off.
  • Be careful as you transition into wind-affected terrain.

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.