Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 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 a collapsible crust exists. Similar structures are also found on westerly-facing slopes. On northerly-facing slopes, these slabs formed over a layer of near-surface facets. Slabs are larger and may be more sensitive at higher elevations due to ongoing 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 wind-loaded terrain and limiting slope angles to less than 35 degrees, without steeper slopes above.
3:23 A pile of large natural avalanches ran on easterly aspects of Purple Ridge last week.