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. As the snowpack adjusts to resent loading events, these weak layers are becoming less reactive. However, skiers and riders still have the potential to trigger these slabs to depths of one to three feet.