Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1.5–2.5
A variety of weak layers exist in the upper 3' of the snowpack (observation). We've found these layers in several snowpits on a variety of aspects (video above/right). They appear to be most problematic on middle and upper elevation sunny slopes where they exist as a crust+facet combination. These layers also exist on shadier aspects where an obvious crust may not be present and where we're occasionally finding surface hoar (photo).
The exact location, makeup, and sensitivity of these layers vary and are difficult to pin down. The complexity and spatial variability of this problem make slope scale stability assessment a highly uncertain task. The safest bet is to assume one or more of these layers exist and are capable of producing a large avalanche.
These layers are slowly healing. Slopes steeper than about 35 degrees, and/or those with recent wind loading will take the longest to stabilize. Therefore, avoiding steep, wind-drifted terrain is an effective way to reduce your odds of triggering a large avalanche.
ADDITIONAL DISCUSSION: You may find sensitive wind drifts at upper elevations. Look for evidence of fresh windblown snow such as drifts, pillows, and new cornice growth. I'd expect these to be small, but given the weak snow surfaces they formed on, they could be sensitive to your weight.