Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 2
The main problem continues to be the poor snowpack structure that exists throughout the entire Wasatch Range. The problem primarily exists on shady slopes at the mid and upper elevations, where a strong slab of snow can release and fail in the weak faceted snow below. Snowpit results, significantly fewer reports of cracking and collapsing and lack of avalanche activity show that the likelihood of triggering an avalanche is decreasing....however, it is still not zero.
Much of our snowpack is made up of varying sizes of weak sugary snow known as facets...or even depth hoar. They're quite beautiful really - often large, angular, crystaline, cupped, even chained sometimes, but they're also quite dangerous when overloaded by heavy snowfall and/or strong winds. If the storm(s) verify, these will be the players in many of the avalanches we see.
Longtime avalanche pro Jake Hutchinson has a nice photo below.