Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Last week's storm formed slabs up to several feet thick over faceted weak layers. Remote triggers and natural avalanches failing on these persistent weak layers have been gradually diminishing since widespread activity peaked last Wednesday. The greatest number of avalanches have occurred on easterly-facing slopes where faceted crusts exist. Similar structures are also found on westerly-facing slopes. On northerly-facing slopes, these slabs formed over a layer of near-surface facets which should be bonding better now. Slabs are larger at higher elevations due to previous wind transport. In a few cases, avalanches have stepped down into older weak layers much deeper in the snowpack, causing destructive avalanches.
Early warning signs for this avalanche problem are rare and feedback is infrequent. You can reduce your chance of triggering this avalanche problem by avoiding recently wind-loaded terrain and unusually shallow terrain. Safer riding is on wind-protected terrain less than 35 degrees, without steeper slopes above.
This large persistent slab ran naturally on the afternoon of 3/28 on Schuylkill Ridge.