Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–3
There is more than one layer of unstable, wind loaded snow that you could trigger today. Both deep (~3ft) and shallow instabilities have been observed recently. The deeper instability rests on a rain crust, which would make an excellent sliding surface for a large avalanche. The shallow instabilities will be easier to trigger, and would still be consequential in the wrong terrain, or could step down to the deeper weak layer. Although recent NE winds have deposited small drifts of snow in unusual places, overall these places have a shallow, unappealing base due to previous wind erosion.