Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2–3
It’s been seven days since a very large avalanche failed on weak layers buried 2-4 feet deep in the Flathead Range. This slide fractured roughly 1500 feet across and ran an estimated 2500 vertical feet. Similar avalanches have been reported in the Flathead Range, southern Glacier Park, and the Whitefish Range since mid-February. These slides ran on aspects NW, through NE, to SE, and above 5000 feet in elevation. Recent avalanches are the most obvious sign of danger.
Although it is becoming more difficult for a rider to trigger an avalanche on buried weak layers, you can still stack the odds in your favor. Do this by digging into the snow to observe and test buried weak layers before committing to steep terrain. You can increase your safety margin by steering around likely trigger points, including wind-scoured or rocky areas–where the weak snow is closer to the surface–or steep roll-overs. Choosing slopes away from overhead hazards, limiting your time above terrain traps, and traveling one at a time in consequential terrain are easy ways to reduce exposure.
(3/8/2023)
The crown of a very large natural avalanche is visible in the upper left of the image, on the lee side of Grant Ridge (map name) on the crest of the Flathead Range. This slide likely ran during the natural avalanche cycle the last full week in February.
Photo: br