Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Upper-elevation slopes may contain weaker snow near a rain crust buried one to two feet deep. The hardness and thickness of the rain crust vary with elevation, and these weak snow grains have proven difficult to trigger in snowpack tests. The additional weight from rain and snow today will add stress to the snow above the rain crust. Rain may also enhance the cohesion of the snow above the crust, forming a stronger slab and increasing the potential for an avalanche on the rain crust.