Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Continued snowfall this week has slowly added stress to the buried weak layer of surface hoar, which is roughly 1 to 2' deep in the Summit Lake area. While we haven't seen any recent avalanches on this layer, we have seen concerning snowpit results in some locations. The most likely place to find this layer is between 2000 to 3000' in sheltered terrain. Sometimes buried surface hoar provides red flags like collapsing or shooting cracks as signs it is unstable. However, it is also possible to trigger an avalanche on this layer without any obvious signs of unstable snow.
To avoid this problem you can always stick to low angle terrain and avoid steep slopes overhead. If you choose to enter steeper terrain you can improve your safety margin by avoiding large start zones and terrain traps like gullies or cliffs in the runout zone. There is a lot of uncertainty about how widespread and how sensitive this weak layer is in Summit Lake, which makes for a challenging decision-making setup. We recommend a conservative mindset to manage the uncertainty with this weak layer.
Wind Slab Avalanches will become likely if winds pick up this afternoon. With plenty of soft snow on the surface from the past few days of snowfall wind slabs can form rapidly at upper elevations.
Loose Snow Avalanches will become more likely if the sun pokes through the clouds today. Be on the lookout for steep solar aspects if the clouds break up during the day, especially on slopes with trees or rocks that will heat up quickly.
Cornice Fall: Cornices have been growing during the active weather over the past week. These can release naturally and may trigger larger avalanches on slopes below. Limit spending time below cornices, and give them plenty of space if you are traveling along ridgelines.
Overnight snowfall in Summit Lake as stormy and unsettled weather continues throughout the area.
Photo: John Sykes