Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Persistent slabs lie upon sun crusts, wind pack, near surface facets and surface hoar at varying depths throughout the snowpack. These potential sliding surfaces formed during previous dry spells, creating a snowpack with poor structure. The likelihood of triggering these slabs to depths of one to three feet will increase during the day with the additional load of the new snow.