Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
At upper elevations where more new, dry snow may fall, check and see how it reacts on steep slopes. Slabs could be more reactive in areas of fresh wind loading, and with warming temperatures we may see an 'upside down' storm layer. Loose dry 'sluffs' may run easily on the crust from Wednesday. You can evaluate how well the new snow is bonding with simple tests like slope cuts, skin track tests, and hand shears.
If you find signs of instabilities like shooting cracks or easy failures with practical tests, than steer away from large, steep, unsupported or consequential slopes.
Example shallow but fairly wide natural soft slab in Rock Mountain's East Bowl.
Photo: Matt Primomo