Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2.5
While ski touring in the Elkhorn mountains yesterday, I dug a snowpit at 8500' on an east facing slope that was 34 degrees steep. Buried 2' down from the surface was a 3/4" thick layer of surface hoar that, at first glance, was hard to find. Even though that layer proved to be unreactive while performing stability tests, it could be tested today if the forecasted 5"-9" of snow and moderate WNW winds materialize. Evaluate carefully any slope steeper than 30 degrees today that you are thinking about traveling on. Dig into the snow and see if you can find buried surface hoar or facet/crust combinations in your snowpit walls. Take the time to perform stability tests. If you are seeing propagation while performing an Extended Column Test, or sudden planar shears on your Compression Tests, these are glaring red flags that instability exists on the steep slope you are considering. Other red flags that warn of snowpack instability include the observance of avalanches, and whumpfing sounds as you are traveling through the terrain. Any red flag observed is a message from the dragon that it is time to get off of and out from under slopes steeper than 30 degrees.
(1/25/2023)
A close up of what buried surface hoar looks like in a snowpit. Can you see the light gray line in this photo ? Surface hoar can be hard to see in certain lighting conditions. Surface hoar is a persistent grain type that causes a large percentage of fatal avalanches once it is buried in the snowpack, and we are seeing a lot of it throughout our forecast area.
Photo: TG