Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Recent Avalanches: Natural wind slabs occurred last week especially towards the beginning of the wind event, but it is difficult to determine where and how big with crowns getting filled in so quickly. There were two human-triggered avalanches in Girdwood last week that are the same type we are concerned with in Summit Lake. These happened in Raggedtop Bowl last Thursday. Check out the reports here and here.
It has been almost 3 weeks since a large avalanche has occurred on the weak snow that formed in Decemberin the Summit Lake area. There are a few reasons why this is still our main concern despite the lack of avalanches.
- Poor structure still exists in the snowpack with a large slab sitting on weak snow. This layer has gained strength over time, but these types of layers are very hard to fully trust and the consequences could be devestating if an avalanche occurs.
- The large avalanches on the north side of the Girdwood area tell us that large avalanches could still occur in the right thin spot with the right load. That side of the Girdwood valley has a similar snowpack to Summit Lake.
We think the chances of a person triggering one of these large avalanches is going down, but there is always some uncertainty with this type of problem. Some things you can do to reduce your exposure and vulnerability include checking safety gear at the parking lot, choosing safe, low angle up routes, avoid riding close to rocks, and travel one at a time in steep terrain while watching partners closely.