Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
The neighboring West North zone had several human-triggered storm slab avalanches on Saturday, and one on Sunday. Conditions there are very similar to much of the West Central zone. The layer we're concerned about is slowly strengthening, but you can still trigger an avalanche on upper-elevation slopes, most likely north-facing, which formed weak layers during the long period of high pressure before the new snow fell. Wind redistributed the weak layer, scrubbing it from ridgetops and possibly redistributing it downslope, resulting in lower crown lines than you might normally see. People are still finding weaknesses and triggering avalanches within the storm snow as well, a few inches to a foot deep. Plenty of graupel was noted during this last storm, contributing to some of these potential sliding layers.
Slopes that are greater than 35° and especially ones that don't provide a smooth runout, aka areas with terrain traps, are locations we recommend avoiding at this time. If you trigger an avalanche you don't want to take a ride through trees or over a cliff. You can also quickly dig down with your hand to the relatively shallow layer to check out how well the layers are bonding before committing to a slope. If you notice whumphing or long shooting cracks these are strong indicators to avoid nearby steep slopes.
(3/14/2023)
A human triggered slab avalanche similar to what you may encounter on Monday.
Photo: Irene Henninger