Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 1.5–2.5
New snow and wind are forming fresh slabs over a thin crust. Recent snow under this crust is well-settled and dense and may remain reactive where it sits over a weak layer of surface hoar on a thicker crust. You can dig down to investigate the bond at these interfaces.