Avalanche forecast

Whitefish Range

Flathead Avalanche Center
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Avalanche danger

Wed
Alpine
2 · Moderate
Treeline
1 · Low
Below
1 · Low
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Out of date — this forecast expired 4 years ago. You’re viewing past conditions, not the current bulletin.

Highlights

Recent strong winds drifted snow into hard slabs on leeward-facing aspects. Slabs will become thicker and more dangerous the higher you climb. Stick to slopes protected from the wind for a safer and better experience.

Avalanche problems

  • Wind Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–2

    Look for and avoid areas where winds drifted snow into firm slabs. These will be more common below ridges and saddles. Keep an eye out for signs of cross-loading further downslope. Wind-drifted snow has a textured appearance and slabs typically have a bulbous or dune shape to them. Seek out slopes with soft snow in areas protected from the wind.

    (2/12/2023)

    A natural avalanche that occurred in the past few days. Steer around or avoid slopes where you see signs of recent wind loading. These will be more common on the downwind of ridgelines. 

    Photo: Burket Kniveton

Avalanche Discussion

Yesterday’s (Monday) storm underproduced in all ranges with remote weather stations showing a trace to 2 inches of snow. What didn’t underproduce were the winds. Mt. Aeneas in the Swan Range averaged speeds of 48 mph for 6 hours yesterday morning. The Whitefish and Flathead/Glacier National Park zones didn’t quite hit those speeds, but still clocked averages between 20 and 35 mph.

Winds had little snow to transport since recent sunny weather capped the surface with a sun crust on south aspects, and sustained winds already transported recent snow. The result of this event is likely a hard, stubborn wind slab on leeward aspects and scoured surfaces on windward aspects. If you decide to go out, head to your most wind-protected locations for a relatively safer experience. Expect to find a new melt-freeze or rain crust at low elevations. 

Mark and Sarah visited a crown from a natural avalanche on Mt. Essex in the Flathead Range. This slab failed at roughly 6000 feet on a northerly aspect. It was a hard slab that slid on top of the Christmas Crust. This is evidence that the poor snowpack structure in the Flathead Range reached a tipping point in areas where winds drifted snow into thicker slabs. For the time being, give areas where winds thickened slabs a wide margin for error to allow this poor structure to adjust to recent loading.

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