Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1
Persistent slabs, which could build to two feet by the end of the day in some places, lie upon a firm crust formed in October. Surface hoar developed on this crust prior to being buried which created a persistent weak layer. As the day progresses, these slabs will become easier to trigger as dense new snow adds weight and temperatures warm. At the mid and upper elevations where the crust exists, backcountry travels could trigger these slides, possibly remotely, and natural activity is not out of the question.