Storm Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1–2
While none of the recent storms have been large by Cascade standards, the snow continues to pile up above our most recent crust. Changes in snow level, precipitation intensity, wind speed, and breaks between systems created several inter-storm layers that could fail and create avalanches. Take time to identify and avoid the features where you are most likely to trigger an avalanche. Steer around convex rollovers, very steep rocky slopes, and areas where the wind drifted the snow into deeper slabs. You can use small inconsequential slopes to test the snow as you travel. Up-track test, small slope cuts, and simple hand-pits can clue you into potential avalanches.
Over the past few days, buried surface hoar and small facets were reported within the upper snowpack. They may exist about 4” (10cm) above a stout crust (12/09). So far we have not seen any avalanches on this layer, but as the slab above them grows, that could change. If you see long shooting cracks or hear whumpfs, dial back your slope angle. Avalanches failing on these weak snow grains can fail in surprising ways and trigger remotely.
(12/15/2020) Example: This natural storm slab occurred at Lanham Creek near Stevens Pass. It failed on a change in snow crystal type within the storm snow. NE aspect 5200' N-SS-D1-I