Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1–2
Strong winds over the past 48hrs have begun to create hard slabs in areas. The leeward sides of ridges, gullies, and /or places that have seen the most wind will have thicker, stiffer slabs. There are two main layers of concern to look out for. One is a layer of basal facets/depth hoar that rests near the ground. We have seen failures on this layer in areas with the shallowest snowpack. The second is a layer of near surface facets that we've generally found living under a decomposing wind crust that was the old snow/new snow interface. You can find this layer in and areas where the snowpack is deepest (North through East). Recent test slopes have all arrested after intial collapse on these layers. Slopes greater than 35 degrees are the most likely to overcome friction and produce an avalanche.
Snow profile for a Northeast aspect just above tree line. Strong pencil hard slab over weak depth hoar.