Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Soft slabs of wind drifted snow from yesterday's westerly winds are the main avalanche problem today. These wind slabs are 1-2 feet thick. The trouble is that they will be stabilizing at different rates. Some may be stubborn and well bonded while others may remain sensitive and can still avalanche.
Photo (M. White) below is from a heavily wind loaded slope along the Park City Ridgeline, South Monitor Bowl, that produced a slide 2 feet deep and 60 feet wide.