Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 3
A persistent weak layer of sugary, faceted snow crystals is buried under a slab 2-4 feet thick. The skier triggered avalanche on Saturday slid on this layer and over two-thirds of our avalanche fatalities involve similarly structured snow with facets like these. About a week ago, avalanches and collapsing were widespread but are now isolated occurrences. This layer is most likely to produce an avalanche at upper elevation slopes facing NW, N, NE and E which had the thickest layer of old snow.
There are many slopes where one might get away with it but there are many where you won't and there are nuances in the snow structure due to slight aspect change that can turn a green light red. It's what led pro observer Mark White to bail two-thirds the way up Bonkers in Broads Fork yesterday. His observation is worth a read. You can find his and many other observations in the menu bar at the top under Observations and Avalanches.
So What to Do? Mark Staples has a good list of options below. They were in his forecast yesterday and I think worth a repeat:
- Ride south-facing slopes where this layer doesn't exist.
- Ride slopes less than 30 degrees in steepness where avalanches generally don't happen.
- If riding northerly facing slopes that are steep enough to slide, choose ones with a clean run-out free of trees and rocks.
- Dig a snowpit. Digging a snowpit may not provide all the answers but it does provide an opportunity to slow down and allow for conversation and decision making among group members.