Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2
Our persistent surface hoar and near-surface facet interface remains a concern, although the interface may be less reactive than a few days prior. Approximately 27" of snow has fallen since the weak layer was buried on 12/8. The most recent signs of instability were shooting cracks, a red flag signs of instability, in White River Canyon on Monday. NWAC public observations reached a fever pitch on Sunday with observers noting the settled slab to be 15-24" in virtually all locations, finding recent widely propagating slabs, and reactivity in some test pits. Most significantly, a skier was caught, carried, partially buried, and strained into trees that day and fortunately was uninjured and self-extracted. Recent reports indicate the weak interface may be gaining strength, becoming harder to identify or get reactive tests on. It's most likely to remain reactive on colder northerly aspects and steep, convex rollovers where the slope drops away from you out of sight. Prudent backcountry travelers will continuously assess this layer as they travel through the terrain, performing multiple hand shears, shovel shears, or better yet shovel tilt tests (see the video). If and only if you are confident that the slab over weak layer structure is NOT present in your terrain, should you consider easing into simple avalanche terrain such as well-supported smaller slopes away from terrain traps such as creeks and gullies.